TY - JOUR AU - Li, Feiyang AU - Wan, Ye AU - Sun, Dongquan AU - Wang, Xiaolin AU - Hu, Wenxuan TI - Determination of the pressure and composition of wet gas fluid inclusions: An in situ Raman spectroscopic approach JF - SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY J2 - SPECTROCHIM ACTA A VL - 308 PY - 2024 PG - 11 SN - 1386-1425 DO - 10.1016/j.saa.2023.123774 UR - https://m2.mtmt.hu/api/publication/34585590 ID - 34585590 AB - Carbonaceous fluid within mineral-hosted inclusions provides important information for carbon cycle in deep Earth. In addition to CH4 and CO2, heavy hydrocarbons (e.g., C2H6 and C3H8) are frequently observed in carbonaceous fluid inclusions (i.e, wet gas inclusions with C-1/& sum;C-i < 0.95). However, determination of the composition of such complex volatiles is difficult based on traditional microthermometric measurements. Here we carried out experimental calibrations on Raman spectroscopic measurements of the pressure (P) and composition of the CH4 +/- C2H6 +/- C3H8 +/- H2S system at room temperature and 0.1-130 MPa. We confirmed that the C-H symmetric stretching vibration band of CH4 [nu(1)(CH4), similar to 2917 cm(-1)] shifted to lower wavenumber with rising pressure, thus the P-nu(1)(CH4) relationship could be applied to calculate the pressure of wet gas. It should be noted that the presence of C-2+ and/or H2S will shift the [nu(1)(CH4)] to lower wavenumber at constant pressure (with the order of C3H8 >= H2S > C2H6). Obviously, the P-nu(1)(CH4) relationship derived from pure CH4 system could not be simply applied to wet gas inclusion, otherwise the pressure would be overestimated. To avoid the overlap of the C-H vibrations of CH4, C2H6 and C3H8, the peak areas and peak heights of the overtone vibration of CH4 [2 nu(4)(CH4), similar to 2580 cm(-1)], C-C symmetric stretching vibrations of C2H6 [nu(3)(C2H6), similar to 995 cm(-1)] and C3H8 [nu(8)(C3H8), similar to 868 cm(-1)], and S-H symmetric stretching vibration of H2S [nu(1)(H2S), similar to 2612 cm(-1)] were fitted using Gaussian + Lorentz functions. The obtained peak areas and peak heights were then used to calculate the Raman quantification factors (F factor and G factor, respectively) of C2H6, C3H8 and H2S relative to CH4, respectively. Both the F factor and G factor increased with rising pressure, whereas the FC2H6, FC3H8 and GH(2)S kept nearly constant at similar to 5.69, 6.39 and 153.8, respectively in high pressure gas mixtures (e.g., >30 MPa). Therefore, for inclusions with higher internal pressure, the molar ratio of CH4, C2H6, C3H8 and H2S could be determined by the aforementioned F and G factors. This method was applied to the calcite-hosted single-phase gas inclusions in the Upper Permian Changxing Formation carbonate reservoir from the eastern Sichuan Basin (South China). Our results indicated that the trapping pressure would be obviously overestimated if the presence of heavy hydrocarbons was not taken into account. LA - English DB - MTMT ER - TY - JOUR AU - Cheng, K. AU - Cui, J. AU - Meng, Z. AU - Liu, J. AU - Kang, Z. AU - Li, J. TI - Characteristics of fluid inclusions and analysis of hydrocarbon accumulation stages of Yan'an Formation in Wuqi area, Ordos Basin JF - ZHONGGUO DIZHI / GEOLOGY IN CHINA J2 - GEO CHINA VL - 50 PY - 2023 IS - 3 SP - 692 EP - 703 PG - 12 SN - 1000-3657 DO - 10.12029/gc20220102001 UR - https://m2.mtmt.hu/api/publication/34112696 ID - 34112696 N1 - Department of Geology, Northwest University, Shaanxi, Xi'an, 710069, China State Key Laboratory of Continental Dynamics, Northwest University, Shaanxi, Xi'an, 710069, China Longdong Shale Oil Development Project Department, Petrochina Changqing Oilfield Company, Gansu, Qingyang, 745000, China Jingbian Oil Production Plant, Yanchang Oilfield Company, Shaanxi, Yulin, 719000, China Export Date: 27 August 2023; Cited By: 0; Correspondence Address: J. Cui; Department of Geology, Northwest University, Xi'an, Shaanxi, 710069, China; email: cuijp@nwu.edu.cn LA - Chinese DB - MTMT ER - TY - JOUR AU - Hasan, Muhammad Luqman AU - M. Tóth, Tivadar TI - Localization of potential migration pathways inside a fractured metamorphic hydrocarbon reservoir using well log evaluation (Mezősas field, Pannonian Basin) JF - GEOENERGY SCIENCE AND ENGINEERING J2 - GEOENERGY SCI ENG VL - 225 PY - 2023 PG - 22 SN - 2949-8929 DO - 10.1016/j.geoen.2023.211710 UR - https://m2.mtmt.hu/api/publication/33720723 ID - 33720723 N1 - Funding Agency and Grant Number: National Research, Development and Innovation Office, Hungary [K-138919] Funding text: Funding This study was supported by the National Research, Development and Innovation Office, Hungary (grant no. K-138919) . LA - English DB - MTMT ER - TY - JOUR AU - Shi, X. AU - Luo, J. AU - Chen, L. AU - Fu, Y. AU - Xu, S. AU - Yan, M. AU - Liu, F. TI - Hydrocarbon Charging Stages and Their Differences in Different Structural Units of the Deep Zhuhai Formation in Wenchang A Sag, Pearl River Mouth Basin JF - DIQIU KEXUE / EARTH SCIENCE: JOURNAL OF CHINA UNIVERSITY OF GEOSCIENCES J2 - EARTH SCI J CHINA UNIV GEOSCI VL - 48 PY - 2023 IS - 2 SP - 776 EP - 792 PG - 17 SN - 1000-2383 DO - 10.3799/dqkx.2022.458 UR - https://m2.mtmt.hu/api/publication/33767199 ID - 33767199 N1 - State Key Laboratory of Continental Dynamics, Northwestern University, Xi'an, 710069, China Zhanjiang Branch of CNOOC Ltd., Zhanjiang, 524057, China Export Date: 23 April 2023 CODEN: DIKEE Correspondence Address: Luo, J.; State Key Laboratory of Continental Dynamics, China; email: jlluo@nwu.edu.cn AB - The Paleogene Zhuhai Formation in the deep Wenchang A Sag of the Pearl River Mouth Basin is rich in oil and gas resources, but the distribution of oil and gas reservoirs in different regions is complex, and the study of inclusions, the key evidence of oil and gas accumulation period, is relatively weak. In order to accurately determine the hydrocarbon charging periods of Zhuhai Formation in Wenchang A Sag, the hydrocarbon inclusions and their associated brine inclusions in the sandstone reservoirs of Zhuhai Formation in the study area were taken as the research object. Fluorescence spectroscopy, laser Raman spectroscopy, micro thermometry and other related experiment were used, combined with the analysis of inclusion capture pressure calculation, burial history, paleogeothermal evolution history, and thermal evolution history of hydrocarbon source rocks. The research on hydrocarbon charging stages and their differences in the central depression and the fault zone has been carried out. The results show that there are three kinds of inclusions, including high‐density single‐phase oil inclusions, two‐phase of gas‐liquid hydrocarbon inclusions and two‐phase of gas‐liquid saline inclusions in the sandstonereservoir. The components of hydrocarbon inclusions and the associated brine inclusions are mainly CH4, C2H6, SO2, CO2 and H2O, and the homogenization temperature of brine inclusions distributed mainly from 95 to 180 ℃. Three stages of hydrocarbon filling occurred both in the central depression and the fault zone, but the hydrocarbon filling time is different. The first hydrocarbon charging occurred in the central depression rangesfrom 21.9 to 13.9 Ma, the second oil filling occurred at 12.0 to 8.9 Ma, and the third oil and gas filling occurred at 7.8 to 4.8 Ma. However, in the fault zone, the first oil charging occurred at 21.7 to 10.2 Ma, the second one occurred at 9.1 to 4.9 Ma, and the third oil and gas filling was about 3.9 to 1.5 Ma. The difference of source rock burial depth, multi‐stage fault activity and their spatio ‐ temporal configuration caused by different tectonic subsidence is the main reason for the difference of hydrocarbon generation peak and hydrocarbon accumulation time in the central depression and fault zone. The research results provide a scientific basis forselection and deployment of oil and gas exploration targets in the study area. © 2023 China University of Geosciences. All rights reserved. LA - Chinese DB - MTMT ER - TY - JOUR AU - Li Qingguang, null AU - Ju Yiwen, null AU - Gu Shangyi, null AU - Wu Pan, null AU - Wu Linna, null AU - Xia Peng, null AU - Yu Kun, null AU - Gao Wei, null AU - Chang Xixi, null TI - Coalbed Methane Accumulation Indicated by Geochemical Evidences from Fracture-filling Minerals in Huaibei coalfield, East China JF - GEOCHEMISTRY INTERNATIONAL J2 - GEOCHEM INT+ VL - 60 PY - 2022 IS - 1 SP - 52 EP - 66 PG - 15 SN - 0016-7029 DO - 10.1134/S001670292113005X UR - https://m2.mtmt.hu/api/publication/32941770 ID - 32941770 N1 - Key Laboratory of Karst Georesources and Environment, Ministry of Education, College of Resource and Environmental Engineering, Guizhou University, Guiyang, 550025, China Key Laboratory of Computational Geodynamics, College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 100049, China Guizhou Research Center of Shale Gas and CBM Engineering Technology, Guizhou Bureau of Coal Geology, Guiyang, 550081, China Export Date: 24 January 2023 Correspondence Address: Yiwen, J.; Key Laboratory of Computational Geodynamics, China; email: juyw03@163.com AB - Fracture-filling minerals in coal-bearing strata are the product of water-rock interactions under specific geological conditions, which reflect the accumulation process and characteristics of CBM enrichment and migration. In this study, vein-bearing sedimentary rock samples from coal-bearing strata in the Huaibei coalfield were selected to reveal the fluid sources and the filling periods of CBM. The carbon source of the vein samples is a mixture of the degraded organic carbon of coal and the dissolution of carbonate minerals in coal measure. Considering the low salinity of the fluid, the infiltration of surface water will also bring some supergenic carbon supplement. Moreover, the high Sr-87/Sr-86 ratios might also be induced by the infiltration of surface water and the dissolution of radiogenic strontium adsorbed in coal. Based on the temperature, salinity, and Raman spectral analysis, the formation of fluid inclusions is divided into two phases: the first phase corresponded to the generation of large-scale thermogenic gas, while the second phase reflected the event of large-scale secondary biogas formation. The values of delta D-CH4 and delta C-13-CH4 in the group inclusions showed that no significant isotope fractionation occurred between the methane in the inclusions and that in the coal seam; the methane in the inclusions is predominantly biogas. This study further reveals the mechanism of CBM formation and accumulation process in the Huaibei coalfield, which could benefit the exploration and development of CBM in this area. LA - English DB - MTMT ER - TY - GEN AU - Yufu, Han TI - Hydrocarbons and NSO-compounds in oil-bearing fluid inclusions detected by FT-ICR-MS and their applications in petroleum systems PY - 2022 DO - 10.14279/depositonce-15541 UR - https://m2.mtmt.hu/api/publication/33591055 ID - 33591055 LA - English DB - MTMT ER - TY - JOUR AU - Zhu, Wei AU - Qi, Yongdi AU - Dai, Shixin AU - Shen, Mingsu TI - Determining the gas accumulation period using fluid inclusion observations: Xiang Zhong Basin, China JF - APPLIED RHEOLOGY J2 - APPL RHEOL VL - 32 PY - 2022 IS - 1 SP - 83 EP - 99 PG - 17 SN - 1430-6395 DO - 10.1515/arh-2022-0126 UR - https://m2.mtmt.hu/api/publication/33167568 ID - 33167568 N1 - School of Earth Sciences and Spatial Information Engineering, Hunan University of Science and Technology, Hunan, Xiangtan, 411201, China Hunan Key Laboratory of Shale Gas Resource Utilization, Hunan, Xiangtan, 411201, China Export Date: 24 January 2023 Correspondence Address: Dai, S.; School of Earth Sciences and Spatial Information Engineering, Hunan, China; email: 8530003@hnust.edu.cn AB - There are a large number of natural gas shows in the Upper Paleozoic of the central Hunan Basin. However, the hydrocarbon accumulation process was complicated due to the strong tectonic reformation in this area. A study of the natural gas accumulation period is of significance for determining gas accumulation models. In this research, the fluid inclusion samples were tested, the fluid inclusion occurrence characteristics, uniform temperature data, and reservoir evolution were analyzed, and four diagenetic periods and four diagenetic periods and three hydrocarbon accumulation periods were identified. (i) For the syntaxial stage, the filling is dark and nonluminous, and the fluid captured by the overgrowing cement around the particles is mainly seawater; (ii) for the (Early) Mesogenetic burial stage, the calcite cement grows around the particles or micritic calcite matrix, and the fluid captured is mainly brine; (iii) for (Late) Mesogenetic burial stage, two sets of decomposed fissures developed in massive calcite colloids with non-luminous gas-rich hydrocarbon inclusions within the crystals; and (iv) for Telogenetic burial stage, weakly fluorescent pure gaseous hydrocarbon inclusions are developed in luminescent calcite veins. The result indicates that the organic inclusions in the Lower Carboniferous of the central Hunan Basin are dominated by weakly fluorescent and nonfluorescent rich gas inclusions and pure gas-phase inclusions, with three stages of hydrocarbon filling. By integrating the average homogenization temperatures on burial curves, the three charging orders correspond to 260-250 Ma during the Late Permian, 249-245 Ma during the Early Triassic, and 208-170 Ma during the Late Triassic. Dense reservoir characteristics reveal deep basin gas reservoir in deep basin. LA - English DB - MTMT ER - TY - JOUR AU - Jayanthi, J. L. AU - Nandakumar, V TI - Fluid inclusion studies to determine the paleotemperature and hydrocarbon quality in petroliferous basins JF - JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING J2 - J PETROL SCI ENG VL - 197 PY - 2021 PG - 10 SN - 0920-4105 DO - 10.1016/j.petrol.2020.108082 UR - https://m2.mtmt.hu/api/publication/31857704 ID - 31857704 N1 - Export Date: 12 February 2021 Correspondence Address: Nandakumar, V.; National Facility for Geofluids Research and Raman Analysis, India; email: nandakumar.v@ncess.gov.in Funding details: Earth System Sciences Organization, Ministry of Earth Sciences, ईएसएसओ Funding text 1: We gratefully acknowledge Oil & Natural Gas Corporation, Govt. of India for their collaboration by providing offshore well cuttings of RV-1 and KK wells as well as the logistic support they provided. The support of Dr. M. Rajeevan (Secretary, Ministry of Earth Sciences, Government of India), and Dr. Shailesh Nayak, (Former Secretary, Ministry of Earth Sciences, Government of India) is gratefully acknowledged. Director, NCESS Dr. P. C. Rao is also acknowledged. Dr. M. Baba, Dr. N. P. Kurian and Dr. V. M. Tiwari (former Directors of CESS/NCESS) are remembered and gratefully acknowledged for their support and encouragement. Cited By :2 Export Date: 12 September 2021 Correspondence Address: Nandakumar, V.; National Facility for Geofluids Research and Raman Analysis, India; email: nandakumar.v@ncess.gov.in Funding details: Ministry of Earth Sciences, एमओईएस Funding details: Earth System Sciences Organization, Ministry of Earth Sciences, ईएसएसओ Funding details: Oil and Natural Gas Corporation, ओएनजीसी Funding text 1: We gratefully acknowledge Oil & Natural Gas Corporation, Govt. of India for their collaboration by providing offshore well cuttings of RV-1 and KK wells as well as the logistic support they provided. The support of Dr. M. Rajeevan (Secretary, Ministry of Earth Sciences, Government of India), and Dr. Shailesh Nayak, (Former Secretary, Ministry of Earth Sciences, Government of India) is gratefully acknowledged. Director, NCESS Dr. P. C. Rao is also acknowledged. Dr. M. Baba, Dr. N. P. Kurian and Dr. V. M. Tiwari (former Directors of CESS/NCESS) are remembered and gratefully acknowledged for their support and encouragement. Funding text 2: We gratefully acknowledge Oil & Natural Gas Corporation, Govt. of India for their collaboration by providing offshore well cuttings of RV-1 and KK wells as well as the logistic support they provided. The support of Dr. M. Rajeevan (Secretary, Ministry of Earth Sciences, Government of India), and Dr. Shailesh Nayak, (Former Secretary, Ministry of Earth Sciences, Government of India) is gratefully acknowledged. Director, NCESS Dr. P. C. Rao is also acknowledged. Dr. M. Baba, Dr. N. P. Kurian and Dr. V. M. Tiwari (former Directors of CESS/NCESS) are remembered and gratefully acknowledged for their support and encouragement. AB - Hydrocarbon bearing fluid inclusions (HCFIs) along with the coeval aqueous inclusions could be utilized in petroleum exploration industry for determining the paleotemperature and American Petroleum Institute's (API) gravity of oils in a basin. These parameters can indirectly yield a quick assessment on the hydrocarbon quality in a basin. Here we use fluid inclusion data as a tool to study the paleotemperature and hydrocarbon quality of two offshore basins in India (dry wells from a proven basin and non-proven basin). Towards this objective, temperature of homogenization (Th) of coeval aqueous fluid inclusion, assemblages seen associated with HCFIs and fluorescence emission features of oils in HCFIs were studied. Depthwise comparison of two basins studied are accorded with the microthermometrically obtained Th data and spectroscopically determined (fluorescence) API gravity values that gives an estimation of the paleotemperature and hydrocarbon quality. The Th and, fluorescence emission features of oils in HCFIs (leads to API gravity) presented allow us to make a qualitative assessment of oils in these basins. This study brings out the potential information stored in HCFIs/adjacent brine fluid inclusions, as a tool for determining the paleotemperature and API gravity of oils in petroliferous basins. LA - English DB - MTMT ER - TY - JOUR AU - Kondor, Henrietta AU - M. Tóth, Tivadar TI - Contrasting metamorphic and post-metamorphic evolutions within the Algyő basement high (Tisza Mega-unit, SE Hungary). Consequences for structural history JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 64 PY - 2021 IS - 2 SP - 91 EP - 112 PG - 22 SN - 1788-2281 DO - 10.1556/24.2021.00004 UR - https://m2.mtmt.hu/api/publication/32055044 ID - 32055044 N1 - Export Date: 12 September 2021 Correspondence Address: KONDOR, H.; Department of Mineralogy Geochemistry and Petrology, Egyetem st. 2, Hungary; email: kondor.henrietta@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Fiser-Nagy, Ágnes AU - Kondor, Henrietta AU - Molnár, László AU - Schubert, Félix AU - Vargáné, Tóth Ilona AU - Zachar, Judit TI - Az Alföld metamorf aljzata: a köztes tömegtől a tarka mozaikig [The metamorphic basement of the great Hungarian plain: From zwischengebirge towards a variegated mosaic] JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 151 PY - 2021 IS - 1 SP - 3 EP - 26 PG - 24 SN - 0015-542X DO - 10.23928/foldt.kozl.2021.151.1.3 UR - https://m2.mtmt.hu/api/publication/31964077 ID - 31964077 N1 - Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) Szegedi Tudományegyetem, Ásványtani, Geokémiai és Kőzettani Tanszék, Egyetem u. 2., Szeged, 6721, Hungary Rhk Kht., Hungary MOL Nyrt., Hungary Export Date: 12 September 2021 LA - Hungarian DB - MTMT ER - TY - BOOK AU - Vivekanandan, Nandakumar AU - J.L., Jayanthi TI - Hydrocarbon Fluid Inclusions in Petroliferous Basins PB - Elsevier CY - Amsterdam PY - 2021 SN - 9780128174173 DO - 10.1016/C2018-0-01344-4 UR - https://m2.mtmt.hu/api/publication/32343986 ID - 32343986 N1 - Cited By :1 Export Date: 23 April 2023 LA - English DB - MTMT ER - TY - JOUR AU - Fu, Sheng AU - Liu, Zhen AU - Zhang, Yi-ming AU - Jiang, Shuan-qi AU - Wang, Xin AU - Wang, Hui-lai AU - Tian, Ning AU - Ya, Hui-li TI - Erosion thickness estimate and hydrocarbon accumulation period of relic basins: A case study of the Wulan-Hua Sag in southern Erlian Basin, NE China JF - GEOLOGICAL JOURNAL J2 - GEOL J VL - 55 PY - 2020 IS - 5 SP - 3430 EP - 3450 PG - 21 SN - 0072-1050 DO - 10.1002/gj.3596 UR - https://m2.mtmt.hu/api/publication/30956587 ID - 30956587 N1 - Funding Agency and Grant Number: Huabei Oilfield, PetroChina Funding text: Huabei Oilfield, PetroChina State Key Laboratory for Petroleum Resources and Prospecting, China University of Petroleum, Beijing, China Huabei Oilfield branch of PetroChina, Renqiu, China Exploration division of Huabei Oilfield branch of PetroChina, China Exploration Development Research Institute of Huabei Oilfield branch of PetroChina, China Export Date: 12 February 2021 Correspondence Address: Liu, Z.; State Key Laboratory for Petroleum Resources and Prospecting, China; email: liuzhenjr@163.com Funding details: PetroChina Company Limited, PetroChina Funding text 1: We thank Huabei Oilfield, PetroChina for their data supports and assistance during the project. State Key Laboratory for Petroleum Resources and Prospecting, China University of Petroleum, Beijing, China Huabei Oilfield branch of PetroChina, Renqiu, China Exploration division of Huabei Oilfield branch of PetroChina, China Exploration Development Research Institute of Huabei Oilfield branch of PetroChina, China Export Date: 12 September 2021 Correspondence Address: Liu, Z.; State Key Laboratory for Petroleum Resources and Prospecting, China; email: liuzhenjr@163.com Funding details: PetroChina Company Limited, PetroChina Funding text 1: We thank Huabei Oilfield, PetroChina for their data supports and assistance during the project. AB - We conducted a study in the Wulan-Hua Sag, a Mesozoic relic sag in the Erlian Basin to analyse and determine the period of its hydrocarbon accumulation. Estimation of erosional thickness is carried out from sonic well logs and seismic velocity data, followed by defining burial history of the Wulan-Hua Sag together with thermal history through basin modelling. Fluid inclusions and pore fluid microthermometric data of 37 samples from clastic reservoir in the Wulan-Hua Sag are available for detailed correlation and analysis. The reconstructed erosion thickness indicates that first of all, differential uplift that is characterized by seesaw uplift-erosion initiated at the north sub-sag. Secondly, largest erosion degree appears in Tumu'er and Saiwusu tectonic belts. Thirdly, the thickness of sedimentary rocks removed by erosion in the south sub-sag progressively increases from its subsiding centre outwardly. Burial history of the Wulan-Hua Sag belongs to type of late-period intensive uplift-erosion. Two types of fluid inclusion are recognized in the Wulan-Hua Sag indicating two hydrocarbon accumulation periods for reservoirs in LK(1)bt(1) (lower interval in first member of Tengge'er Formation), which is middle depositing period of K(1)bt(1) (first member of Tengge'er Formation) to early depositing period of K(1)bt(2) (second member of Tengge'er Formation) and early K(1)bt(2) to middle K(1)bs (Saihantala Formation) depositing period, respectively. Reservoir in the K(1)ba and upper interval of K(1)bt(1) appears to have experienced one hydrocarbon accumulation period, which is early K(1)bt(1) to early K(1)bt(2) depositing period. And reservoir in the UK(1)bt(1) (upper interval in first member of Tengge'er Formation) also has one hydrocarbon accumulation period, which is late K(1)bt(2) depositing period to the Late Cretaceous (K-2). Hydrocarbon accumulation model of the Wulan-Hua Sag consists of two oil-reservoir types including "upward-charging" and "self-sourced." Reservoir in lower interval of K(1)bt(1) and reservoir in the upper interval of K(1)bt(1) are considered to have more hydrocarbon exploration potential. LA - English DB - MTMT ER - TY - JOUR AU - Laczkó-Dobos, Emese AU - Gier, S AU - Sztanó, Orsolya AU - Milovský, R AU - Hips, Kinga TI - Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary) JF - GEOFLUIDS J2 - GEOFLUIDS VL - 2020 PY - 2020 PG - 26 SN - 1468-8115 DO - 10.1155/2020/9020684 UR - https://m2.mtmt.hu/api/publication/31783545 ID - 31783545 N1 - Eötvös Loránd University, Pázmány Péter sétány 1/c, Budapest, 1117, Hungary MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/c, Budapest, H -1117, Hungary Department of Geodynamics and Sedimentology, Universität Wien, Austria Earth Science Institute of the Slovak Academy of Sciences, Banská Bystrica, Ďumbierska, Slovakia Cited By :1 Export Date: 4 July 2022 Correspondence Address: Laczkó-Dobos, E.; Eötvös Loránd University, Pázmány Péter sétány 1/c, Hungary; email: meseszocs@caesar.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Liu, Dongdong AU - Zhang, Chen AU - Pan, Zhankun AU - Huang, Zhixin AU - Luo, Qun AU - Song, Yan AU - Jiang, Zhenxue TI - Natural fractures in carbonate-rich tight oil reservoirs from the Permian Lucaogou Formation, southern Junggar Basin, NW China: Insights from fluid inclusion microthermometry and isotopic geochemistry JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 119 PY - 2020 PG - 15 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2020.104500 UR - https://m2.mtmt.hu/api/publication/31432821 ID - 31432821 N1 - Funding Agency and Grant Number: National Science and Technology Major Project [2016ZX05034-001, 2017ZX05035-002]; National Key R&D Program of China [2015CB250901] Funding text: We would like to express our gratitude to John N. Hooker and two anonymous reviewers for their critical reviews and constructive comments for the earlier version of this manuscript. This work was financially supported by National Science and Technology Major Project (2016ZX05034-001, 2017ZX05035-002), and National Key R&D Program of China (2015CB250901). State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum Beijing, Beijing, 102249, China Unconventional Petroleum Research Institute, China University of Petroleum Beijing, Beijing, 102249, China College of Geosciences, China University of Petroleum Beijing, Beijing, 102249, China Cited By :1 Export Date: 12 February 2021 Correspondence Address: Liu, D.; State Key Laboratory of Petroleum Resources and Prospecting, China; email: liudd@cup.edu.cn Funding details: 2015CB250901 Funding details: Science and Technology Major Project of Guangxi, 2017ZX05035-002, 2016ZX05034-001 Funding text 1: We would like to express our gratitude to John N. Hooker and two anonymous reviewers for their critical reviews and constructive comments for the earlier version of this manuscript. This work was financially supported by National Science and Technology Major Project ( 2016ZX05034-001 , 2017ZX05035-002 ), and National Key R&D Program of China ( 2015CB250901 ). State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum Beijing, Beijing, 102249, China Unconventional Petroleum Research Institute, China University of Petroleum Beijing, Beijing, 102249, China College of Geosciences, China University of Petroleum Beijing, Beijing, 102249, China Cited By :5 Export Date: 12 September 2021 Correspondence Address: Liu, D.; State Key Laboratory of Petroleum Resources and Prospecting, China; email: liudd@cup.edu.cn Funding details: National Key Research and Development Program of China, NKRDPC, 2015CB250901 Funding details: National Major Science and Technology Projects of China, 2016ZX05034-001, 2017ZX05035-002 Funding details: Science and Technology Major Project of Guangxi Funding text 1: We would like to express our gratitude to John N. Hooker and two anonymous reviewers for their critical reviews and constructive comments for the earlier version of this manuscript. This work was financially supported by National Science and Technology Major Project ( 2016ZX05034-001 , 2017ZX05035-002 ), and National Key R&D Program of China ( 2015CB250901 ). Funding text 2: We would like to express our gratitude to John N. Hooker and two anonymous reviewers for their critical reviews and constructive comments for the earlier version of this manuscript. This work was ?nancially supported by National Science and Technology Major Project (2016ZX05034-001, 2017ZX05035-002), and National Key R&D Program of China (2015CB250901). AB - Natural fractures within tight reservoirs form preferred pathways for hydrocarbon charge and provide space for hydrocarbon preservation. However, the mechanism that controls the formation of natural fractures in tight reservoirs remains controversial. This study investigates natural fractures within carbonate-rich tight oil reservoirs from the Permian Lucaogou Formation in the Jimsar Sag, southern Junggar Basin. Drill core and image log observations show that fractures in the Lucaogou Formation can be categorized into two types: beddingparallel fractures and inclined fractures. The carbon and oxygen isotopic compositions of calcite cements in the bedding-parallel fractures range from 0.6 parts per thousand to 6.0 parts per thousand (delta C-13(PDB)), and from -15.5 parts per thousand to -8.9 parts per thousand (delta O-18(PDB)), respectively, which are similar to those of the organic-rich host rock. This suggests that the bedding-parallel fractures likely formed in a closed fluid system. Fluid inclusion analyses of the aqueous inclusions in calcite cements from the bedding-parallel fractures record homogenization temperatures of 91.5 degrees C-130.4 degrees C, indicating that they formed at the Cretaceous to Cenozoic, during when the Lucaogou Formation reached peak oil generation stage. Therefore, the bedding-parallel fractures were most likely generated by hydrocarbon generation overpressure. The presence of hydrocarbon inclusions in bedding-parallel fracture cements supports natural fracturing by high pore-fluid pressure. The delta C-13(PDB) and delta O-18(PDB) of calcite cements within the inclined fractures vary from 3.6 parts per thousand to 9.6 parts per thousand, and from -11.0 parts per thousand to -2.9%, respectively, which are close to those of the carbonaterich parent rock. This also supports a closed fluid system scenario. The relatively lower fluid inclusion trapping temperatures (70.5 degrees C-109.7 degrees C) suggest that they were likely generated by decrease of confining stress during uplift processes. Therefore, both an increase in pore-fluid pressure and a decrease in confining stress contribute to the formation of natural fractures in the Lucaogou Formation tight oil reservoirs. LA - English DB - MTMT ER - TY - JOUR AU - Liu, Guoping AU - Zeng, Lianbo AU - Han, Chunyuan AU - Ostadhassan, Mehdi AU - Lyu, Wenya AU - Wang, Qiqi AU - Zhu, Jiangwei AU - Hou, Fengxiang TI - Natural Fractures in Carbonate Basement Reservoirs of the Jizhong Sub-Basin, Bohai Bay Basin, China: Key Aspects Favoring Oil Production JF - ENERGIES J2 - ENERGIES VL - 13 PY - 2020 IS - 18 PG - 23 SN - 1996-1073 DO - 10.3390/en13184635 UR - https://m2.mtmt.hu/api/publication/31725808 ID - 31725808 N1 - Funding Agency and Grant Number: National Major Science and Technology Projects of China [2017ZX05008-006-002-005] Funding text: This research was funded by the National Major Science and Technology Projects of China, grant number 2017ZX05008-006-002-005. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249, China College of Geosciences, China University of Petroleum (Beijing), Beijing, 102249, China PetroChina Huabei Oilfield Company, Cangzhou, 062552, China Department of Petroleum Engineering, University of North Dakota, Grand Forks, ND 58202, United States Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78713, United States Export Date: 12 February 2021 Correspondence Address: Zeng, L.; State Key Laboratory of Petroleum Resources and Prospecting, China; email: lbzeng@sina.com Funding details: National Major Science and Technology Projects of China, 2017ZX05008-006-002-005 Funding text 1: Funding: This research was funded by the National Major Science and Technology Projects of China, grant number 2017ZX05008-006-002-005. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249, China College of Geosciences, China University of Petroleum (Beijing), Beijing, 102249, China PetroChina Huabei Oilfield Company, Cangzhou, 062552, China Department of Petroleum Engineering, University of North Dakota, Grand Forks, ND 58202, United States Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78713, United States Cited By :1 Export Date: 12 September 2021 Correspondence Address: Zeng, L.; State Key Laboratory of Petroleum Resources and Prospecting, China; email: lbzeng@sina.com Funding details: China University of Petroleum, Beijing, CUPB Funding details: National Major Science and Technology Projects of China, 2017ZX05008-006-002-005 Funding text 1: The authors greatly acknowledge the Petro China Huabei Oilfield Company for providing information and other support. The authors would also like to thank the work made by Li Jian and Lyu Peng in the China University of Petroleum-Beijing, which enabled our study to proceed successfully. We are also particularly grateful to Veljko Pajovic and three anonymous reviewers for providing constructive comments and suggestions, which improve our manuscript significantly. Funding text 2: Funding: This research was funded by the National Major Science and Technology Projects of China, grant number 2017ZX05008-006-002-005. AB - Analysis of natural fractures is essential for understanding the heterogeneity of basement reservoirs with carbonate rocks since natural fractures significantly control key attributes such as porosity and permeability. Based on the observations and analyses of outcrops, cores, borehole image logs, and thin sections from the Mesoproterozoic to Lower Paleozoic in the Jizhong Sub-Basin, natural fractures are found to be abundant in genetic types (tectonic, pressure-solution, and dissolution) in these reservoirs. Tectonic fractures are dominant in such reservoirs, and lithology, mechanical stratigraphy, and faults are major influencing factors for the development of fractures. Dolostones with higher dolomite content are more likely to have tectonic fractures than limestones with higher calcite content. Most tectonic fractures are developed inside mechanical units and terminate at the unit interface at nearly perpendicular or high angles. Also, where a thinner mechanical unit is observed, tectonic fractures are more frequent with a small height. Furthermore, the dominant direction of tectonic fractures is sub-parallel to the fault direction or oblique at a small angle. In addition, integrating diverse characteristics of opening-mode fractures and well-testing data with oil production shows that, in perforated intervals where dolostone and limestone are interstratified or dolostone is the main lithologic composition, fractures are developed well, and the oil production is higher. Moreover, fractures with a larger dip angle have bigger apertures and contribute more to oil production. Collectively, this investigation provides a future reference for understanding the importance of natural fractures and their impact on oil production in the carbonate basement reservoirs. LA - English DB - MTMT ER - TY - JOUR AU - Liu, Guoping AU - Zeng, Lianbo AU - Li, Hongnan AU - Ostadhassan, Mehdi AU - Rabiei, Minou TI - Natural fractures in metamorphic basement reservoirs in the Liaohe Basin, China JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 119 PY - 2020 PG - 15 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2020.104479 UR - https://m2.mtmt.hu/api/publication/31432823 ID - 31432823 N1 - State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249, China College of Geosciences, China University of Petroleum (Beijing), Beijing, 102249, China Research Institute of Petroleum Exploration and Development, Liaohe Oilfield Company, PetroChina, Panjin, Liaoning 124010, China Department of Petroleum Engineering, University of North Dakota, Grand Forks, ND 58202, United States Cited By :3 Export Date: 12 February 2021 Correspondence Address: Zeng, L.; China University of Petroleum (Beijing), 18 Fuxue Road, Changping, China; email: lbzeng@sina.com Funding text 1: The authors greatly acknowledge the PetroChina Liaohe Oilfield Company for their help in providing information and other support. The authors would also like to thank the works made by Professor Peng Shimi in China University of Petroleum-Beijing, and Ms. He Shuting in PetroChina Liaohe Oilfield exploration and development research institute, which has enabled our work to proceed smoothly. We are particularly grateful to JMPG Associate Editor Dr. Nicolas Beaudoin and two anonymous reviewers for their constructive comments, which contributed significantly to the improvement of the manuscript. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249, China College of Geosciences, China University of Petroleum (Beijing), Beijing, 102249, China Research Institute of Petroleum Exploration and Development, Liaohe Oilfield Company, PetroChina, Panjin, Liaoning 124010, China Department of Petroleum Engineering, University of North Dakota, Grand Forks, ND 58202, United States Cited By :5 Export Date: 12 September 2021 Correspondence Address: Zeng, L.; China University of Petroleum (Beijing), 18 Fuxue Road, Changping, China; email: lbzeng@sina.com Funding text 1: The authors greatly acknowledge the PetroChina Liaohe Oilfield Company for their help in providing information and other support. The authors would also like to thank the works made by Professor Peng Shimi in China University of Petroleum-Beijing, and Ms. He Shuting in PetroChina Liaohe Oilfield exploration and development research institute, which has enabled our work to proceed smoothly. We are particularly grateful to JMPG Associate Editor Dr. Nicolas Beaudoin and two anonymous reviewers for their constructive comments, which contributed significantly to the improvement of the manuscript. AB - The Archaean metamorphic basement reservoirs that are characterized by the development of natural fractures are the primary target for oil and gas exploration in the Liaohe Basin. Based on the analyses of outcrops, cores, thin sections, imaging logs, and laboratory measurements, tectonic fractures are the dominant type of natural fractures, and their development is mainly influenced by petrology and faulting. Tectonic fractures are more developed in metamorphic rocks with a higher content of brittle minerals, while fracture orientations are primarily parallel or almost parallel to the fault strikes. Opening-mode fractures, which account for more than 65% of the total reservoir porosity, provide the primary storage space for metamorphic basement reservoirs. Besides, opening-mode fractures serve as the major pathways for fluid flow throughout the reservoirs and ultimately determine the quality of these reservoirs. Therefore, the discrepancies in fracture development are speculated to be the primary reason leading to the vertical stratification of reservoirs. According to the degree of fracture development, various rock types in metamorphic basement reservoirs can be arranged in order as leptite, granulite, migmatitic granite, gneiss, lamprophyre, diabase, and amphibolite. In this sequence, the former rocks are more likely to become effective reservoirs, while the latter ones are usually inner interlayers. However, the lithology boundary of reservoir rocks and inner interlayers is not definite in this sequence. In a specific metamorphic basement reservoir, the rocks that can become reservoirs have a lower limit in the sequence. But for numerous metamorphic basement reservoirs in the Liaohe Basin, there is no lower limit for rocks to become hydrocarbon-bearing reservoirs. LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Vargáné Tóth, I TI - Lithologically controlled behaviour of the Dorozsma metamorphic hydrocarbon reservoir (Pannonian Basin, SE Hungary) JF - JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING J2 - J PETROL SCI ENG VL - 195 PY - 2020 PG - 16 SN - 0920-4105 DO - 10.1016/j.petrol.2020.107748 UR - https://m2.mtmt.hu/api/publication/31614407 ID - 31614407 N1 - Cited By :1 Export Date: 12 February 2021 Correspondence Address: M Tóth, T.; University of Szeged, Hungary; email: mtoth@geo.u-szeged.hu Funding text 1: The authors thank Enago (www.enago.com) for the English language review. Three anonymous reviewers are thanked for their valuable comments. Cited By :3 Export Date: 12 September 2021 Correspondence Address: M Tóth, T.; University of Szeged, Hungary; email: mtoth@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Molnár, László AU - Körmös, Sándor AU - Czirbus, Nóra AU - Schubert, Félix TI - Localisation of Ancient Migration Pathways inside a Fractured Metamorphic Hydrocarbon Reservoir in South-East Hungary JF - APPLIED SCIENCES-BASEL J2 - APPL SCI-BASEL VL - 10 PY - 2020 IS - 20 PG - 20 SN - 2076-3417 DO - 10.3390/app10207321 UR - https://m2.mtmt.hu/api/publication/31646840 ID - 31646840 N1 - Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Szeged, 6720, Hungary Public Limited Company for Radioactive Waste Management (PURAM), Budapest, 2040, Hungary Export Date: 11 February 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Hungary; email: mtoth@geo.u-szeged.hu Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Szeged, 6720, Hungary Public Limited Company for Radioactive Waste Management (PURAM), Budapest, 2040, Hungary Export Date: 12 February 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Hungary; email: mtoth@geo.u-szeged.hu Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Szeged, 6720, Hungary Public Limited Company for Radioactive Waste Management (PURAM), Budapest, 2040, Hungary Export Date: 18 April 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Hungary; email: mtoth@geo.u-szeged.hu Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Szeged, 6720, Hungary Public Limited Company for Radioactive Waste Management (PURAM), Budapest, 2040, Hungary Export Date: 12 September 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Hungary; email: mtoth@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Tian, Tao AU - Yang, Peng AU - Ren, Zhanli AU - Fu, Deliang AU - Zhou, Shixin AU - Yang, Fu AU - Li, Jing TI - Hydrocarbon migration and accumulation in the Lower Cambrian to Neoproterozoic reservoirs in the Micangshan tectonic zone, China: New evidence of fluid inclusions JF - ENERGY REPORTS J2 - ENERGY REP VL - 6 PY - 2020 SP - 721 EP - 733 PG - 13 SN - 2352-4847 DO - 10.1016/j.egyr.2020.03.012 UR - https://m2.mtmt.hu/api/publication/31857705 ID - 31857705 N1 - Funding Agency and Grant Number: Open Found of Shandong Key Laboratory of Depositional Mineralization and Sedimentary Minerals [DMSM20190022]; Independent Project of Key Laboratory of Coal Exploration and Comprehensive Utilization, Ministry of Natural Resources [ZP2019-2]; State Key Program of National Natural Science Foundation of ChinaNational Natural Science Foundation of China (NSFC) [41630312]; National Science and Technology Major Project [2016ZX05003002-004, 2016B-05-02] Funding text: This study was supported by the Open Found of Shandong Key Laboratory of Depositional Mineralization and Sedimentary Minerals (Grant No. DMSM20190022), the Independent Project of Key Laboratory of Coal Exploration and Comprehensive Utilization, Ministry of Natural Resources (Grant No. ZP2019-2), the State Key Program of National Natural Science Foundation of China (Grant No. 41630312) and National Science and Technology Major Project (Grant Nos. 2016ZX05003002-004 and 2016B-05-02) Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Natural Resources, Xián, 710021, China Shandong Key Laboratory of Depositional Mineralization & Sedimentary Minerals, Shandong University of Science and Technology, Qingdao, 266590, China State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, 710069, China Lanzhou Center for Oil and Gas Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Lanzhou, 73000, China Cited By :3 Export Date: 12 February 2021 Correspondence Address: Yang, P.; Department of Geology Northwest University, Taibai Road No.229, China; email: p.yang@nwu.edu.cn Funding details: DMSM20190022 Funding details: Science and Technology Major Project of Guangxi, 2016B-05-02, 2016ZX05003002-004 Funding details: Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Land and Resources, CRECU, MLR, ZP2019-2 Funding details: National Natural Science Foundation of China, NSFC, 41630312 Funding text 1: This study was supported by the Open Found of Shandong Key Laboratory of Depositional Mineralization and Sedimentary Minerals (Grant No. DMSM20190022 ), the Independent Project of Key Laboratory of Coal Exploration and Comprehensive Utilization, Ministry of Natural Resources (Grant No. ZP2019-2 ), the State Key Program of National Natural Science Foundation of China (Grant No. 41630312 ) and National Science and Technology Major Project (Grant Nos. 2016ZX05003002-004 and 2016B-05-02 ) Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Natural Resources, Xián, 710021, China Shandong Key Laboratory of Depositional Mineralization & Sedimentary Minerals, Shandong University of Science and Technology, Qingdao, 266590, China State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, 710069, China Lanzhou Center for Oil and Gas Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Lanzhou, 73000, China Cited By :4 Export Date: 12 September 2021 Correspondence Address: Yang, P.; Department of Geology Northwest University, Taibai Road No.229, China; email: p.yang@nwu.edu.cn Funding details: DMSM20190022 Funding details: National Natural Science Foundation of China, NSFC, 41630312 Funding details: Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Land and Resources, CRECU, MLR, ZP2019-2 Funding details: Science and Technology Major Project of Guangxi, 2016B-05-02, 2016ZX05003002-004 Funding text 1: This study was supported by the Open Found of Shandong Key Laboratory of Depositional Mineralization and Sedimentary Minerals (Grant No. DMSM20190022 ), the Independent Project of Key Laboratory of Coal Exploration and Comprehensive Utilization, Ministry of Natural Resources (Grant No. ZP2019-2 ), the State Key Program of National Natural Science Foundation of China (Grant No. 41630312 ) and National Science and Technology Major Project (Grant Nos. 2016ZX05003002-004 and 2016B-05-02 ) AB - The Lower Paleozoic reservoir in the Micangshan tectonic zone is a new shale gas exploration area with excellent potential. However, the hydrocarbon migration and accumulation histories of this reservoir have not been thoroughly elucidated and urgently require further research. Fluid inclusions offer a unique and useful method to test for hydrocarbon migration, accumulation, composition and timing. This study integrated the hydrocarbon charge history using fluid inclusions in the Lower Cambrian to Neoproterozoic reservoir from the Micangshan tectonic zone. This work involves the delineation and analysis of fluid inclusions using the petrography, spectroscopy and microthermometry of fluid inclusions. Based on the fluid inclusion analyses combined with reservoir thermal history, timing estimates and charge models of the hydrocarbons were obtained. The formation of natural gas was multifactorial in the Lower Cambrian to Neoproterozoic petroleum system, and the gas in the Niutitang (epsilon(1)n) and Dengying (Z(2)d) reservoirs was mainly from oil cracking and dry gas, and gas in the Xiannvdong (epsilon(1)x) and Canglangpu (epsilon(1)c) reservoirs was abiogenic and formed in hydrothermal fluids by regional tectonothermal events. Three well-defined stages of hydrocarbon charge were identified in the petroleum system in the Micangshan tectonic zone. The stage of oil charge first began before the Early Permian (similar to 277 Ma); the stage of gas charge from oil cracking occurred in the Late Triassic to Early Jurassic (212 Ma-198 Ma); and the stage of gas charge from dry gas occurred in the Middle Jurassic (173 Ma-166 Ma). The gas of mixed origin from the Niutitang reservoir was stored in the nanoscale pores as a self-reservoir, rather than as an effective gas source for the overlying reservoirs. (C) 2020 The Authors. Published by Elsevier Ltd. LA - English DB - MTMT ER - TY - JOUR AU - Xue, N. AU - Zhu, G.-Y. AU - Lü, X.-X. AU - He, T. AU - Wu, Z.-H. TI - Advances in geochronology of hydrocarbon accumulation JF - NATURAL GAS GEOSCIENCE J2 - NATURAL GAS GEOSCIENCE VL - 31 PY - 2020 IS - 12 SP - 1733 EP - 1748 PG - 16 SN - 1672-1926 DO - 10.11764/j.issn.1672-1926.2020.07.004 UR - https://m2.mtmt.hu/api/publication/32191764 ID - 32191764 N1 - State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249, China PetroChina Research Institute of Petroleum Exploration & Development, Beijing, 100083, China Export Date: 12 September 2021 Correspondence Address: Zhu, G.-Y.; PetroChina Research Institute of Petroleum Exploration & DevelopmentChina; email: zhuguangyou@petrochina.com.cn Funding details: 2018A-0102, 2019B-04 Funding details: National Key Research and Development Program of China, NKRDPC Funding details: National Major Science and Technology Projects of China, 2017 ZX05005002-005 Funding text 1: Abstract：Timing technology for oil and gas transportation and accumulation（dating or determining the hydro‐ carbon accumulation period）is a very critical technology in the study of oil and gas from a series of processes such as hydrocarbon generation，migration，accumulation，and preservation. Whether it is for optimizing explo‐ ration targets，reconstructing the formation and evolution process of oil and gas reservoirs，or for enriching and deepening the theory of oil and gas accumulation，it has very important practical and theoretical significance. In the past few decades，scholars at home and abroad have conducted a large number of exploratory studies on the dating of hydrocarbon accumulation，and gradually formed the petroleum accumulation geochronology. As a branch of petroleum geology，based on systematic investigations，the author believes that the formation and de‐ velopment of petroleum accumulation geochronology has gone through three main stages：qualitative description stage，semi-quantitative description stage，quantitative characterization stage. By summarizing and categoriz‐ ing，it is mainly divided into traditional geological analysis method，fluid inclusion dating method and isotope dating method，and the application principle，scope of application，advantages and disadvantages of various dat‐ ing methods are briefly introduced. Key words：Hydrocarbon accumulation dating；Quantitative description；Fluid inclusion dating；Isotopic dating Foundation items：The Scientific Research and Technology Development Project of PetroChina（Grant Nos. 2019B-04，2018A-0102）；The China National Science and Technology Major Project（Grant No. 2017 ZX05005002-005）. Funding text 2: The Scientific Research and Technology Development Project of PetroChina(2019B-04);The China National Science and Technology Major Project(2017 ZX05005002-005). AB - Timing technology for oil and gas transportation and accumulation (dating or determining the hydrocarbon accumulation period) is a very critical technology in the study of oil and gas from a series of processes such as hydrocarbon generation, migration, accumulation, and preservation. Whether it is for optimizing exploration targets, reconstructing the formation and evolution process of oil and gas reservoirs, or for enriching and deepening the theory of oil and gas accumulation, it has very important practical and theoretical significance. In the past few decades, scholars at home and abroad have conducted a large number of exploratory studies on the dating of hydrocarbon accumulation, and gradually formed the petroleum accumulation geochronology. As a branch of petroleum geology, based on systematic investigations, the author believes that the formation and development of petroleum accumulation geochronology has gone through three main stages: qualitative description stage, semi-quantitative description stage, quantitative characterization stage. By summarizing and categorizing, it is mainly divided into traditional geological analysis method, fluid inclusion dating method and isotope dating method, and the application principle, scope of application, advantages and disadvantages of various dating methods are briefly introduced. © 2020, Science Press. All right reserved. LA - Chinese DB - MTMT ER - TY - JOUR AU - Konert, G AU - Steinbach, Gábor AU - Canonico, M AU - Kaňa, R TI - Protein Arrangement (PA) factor. a new photosynthetic parameter characterizing the organization of thylakoid membrane proteins. TS - a new photosynthetic parameter characterizing the organization of thylakoid membrane proteins. JF - PHYSIOLOGIA PLANTARUM J2 - PHYSIOL PLANTARUM VL - 166 PY - 2019 IS - 1 SP - 264 EP - 277 PG - 14 SN - 0031-9317 DO - 10.1111/ppl.12952 UR - https://m2.mtmt.hu/api/publication/30642264 ID - 30642264 N1 - Institute of Microbiology, CAS, Centrum Algatech, Třeboň, Czech Republic Institute of Biophysics, Biological Research Center, Szeged, Hungary Cited By :5 Export Date: 12 September 2021 CODEN: PHPLA Correspondence Address: Kaňa, R.; Institute of Microbiology, Czech Republic; email: kana@alga.cz Chemicals/CAS: Photosystem I Protein Complex; Photosystem II Protein Complex; Phycobilisomes; Thylakoid Membrane Proteins Funding details: CZ 1.05/2.1.00/19.0392, GACR 16-10088S, MSMT LO1416 Funding text 1: Acknowledgements – This research project was supported by The Czech Science Foundation GACˇ R (Grantová agen-tura Cˇ eské republiky) project GACR 16-10088S. The work at center ALGATECH has been supported by the institutional projects Algatech Plus (MSMT LO1416) and Algamic (CZ 1.05/2.1.00/19.0392) from the Czech Ministry of Education, Youth and Sport. We thank Minna Koskela and Eliška Kuthanová (in scientific field known as Trsková or Trsková-Kuthanová) for critical reading of the manuscript and Janos Farkas for analyzing preliminary experimental data and Filip Charvát for the setup of PAM instruments and for additional measurements of cell physiology. We want to thank Adéla Straškova for designing and carrying out preliminary experiments with PSI-YFP-tagged Synechocystis cells during HL stress. AB - A proper spatial distribution of photosynthetic pigment-protein complexes - PPCs (photosystems, light-harvesting antennas) is crucial for photosynthesis. In plants, photosystems (PSI and PSII) are heterogeneously distributed between granal and stromal thylakoids. Here we have described similar heterogeneity in the PSI, PSII, and Phycobilisomes (PBS) distribution in cyanobacteria thylakoids into microdomains by applying a new image processing method suitable for the Synechocystis sp. PCC6803 strain with YFP-tagged PSI. The new image processing method is able to analyze fluorescence ratios of PPCs on single cell level, pixel per pixel. Each cell pixel is plotted in CIE1931 color space by forming a pixel-color distribution of the cell. The most common position in CIE1931 is then defined as protein arrangement (PA) factor with x-y coordinates. The PA-factor represents the most abundant fluorescence ratio of PSI/PSII/PBS, the "mode color" of studied cell. We proved that a shift of the PA-factor from the center of the cell-pixel distribution (the "median" cell color) is an indicator of the presence of special subcellular microdomain(s) with a unique PSI/PSII/PBS fluorescence ratio in comparison to other parts of the cell. Further, during a 6 hour high-light (HL) treatment, "median" and "mode" color (PA-factor) of the cell changed similarly on the population level, indicating that such microdomains with unique PSI/PSII/PBS fluorescence were not formed during HL (i.e. fluorescence changed equally in the whole cell). However, the PA-factor was very sensitive in characterizing fluorescence ratios of PSI/PSII/PBS in cyanobacterial cells during HL by depicting a 4-phase acclimation to HL and their physiological interpretation has been discussed. This article is protected by copyright. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Levresse, Gilles AU - Tritlla, Jordi AU - Ramos Rosique, Aldo AU - Cardellach, Esteve AU - Rollion-Bard, Claire AU - Pironon, Jacques AU - Jimenez Sandoval, Sergio TI - Hydrocarbons in silica: PVTX properties of fluids and the genesis of diamond quartz from Caravia-Berbes Fluorite district (Asturias, Spain) JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 102 PY - 2019 SP - 1 EP - 15 PG - 15 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2018.11.039 UR - https://m2.mtmt.hu/api/publication/30956585 ID - 30956585 N1 - Funding Agency and Grant Number: UNAM-PAPIITPrograma de Apoyo a Proyectos de Investigacion e Innovacion Tecnologica (PAPIIT)Universidad Nacional Autonoma de Mexico [IN100707, IN109410-3]; CONACYTConsejo Nacional de Ciencia y Tecnologia (CONACyT) [81584] Funding text: Special thanks to Marina Vega, Juan Tomas Vasquez Perez and Teresa Soledad Medina Malagon for their assistance at the CGEO laboratory. This study was financed by UNAM-PAPIIT projects IN100707, IN109410-3 and CONACYT project 81584. Programa de Geofluidos, Centro de Geociencias UNAM-Campus Juriquilla, AP 1-253, Querétaro, Mexico 76230, Mexico Repsol Exploración S.A., Méndez Alvaro 44, Madrid, 28045, Spain Departament de Géologia, Facultat de Ciències, Universitat Autònoma de Barcelona, Bellaterra, Barcelona, 08193, Spain Centre de Recherches Pétrographiques et Géochimiques, UMR7358, 15 rue Notre Dame des Pauvres, Vandoeuvre-lès-Nancy Cédex, F-54 501, France Université de Lorraine, CNRS, CREGU, GeoRessources UMR 7359, BP 70239, Vandoeuvre-lès-Nancy, F-54506, France Centro de Investigación y de Estudios Avanzados del Instituto Politecnico Nacional, Unidad Querétaro, Apartado Postal 1-798, Querétaro, Qro 76001, Mexico Cited By :2 Export Date: 12 February 2021 Correspondence Address: Levresse, G.; Programa de Geofluidos, AP 1-253, Mexico; email: glevresse@geociencias.unam.mx Funding details: Consejo Nacional de Ciencia y Tecnología, CONACYT, 81584 Funding details: IN109410-3, IN100707 Funding text 1: Special thanks to Marina Vega, Juan Tomas Vasquez Perez and Teresa Soledad Medina Malagón for their assistance at the CGEO laboratory. This study was financed by UNAM-PAPIIT projects IN100707 , IN109410-3 and CONACYT project 81584 . Programa de Geofluidos, Centro de Geociencias UNAM-Campus Juriquilla, AP 1-253, Querétaro, Mexico 76230, Mexico Repsol Exploración S.A., Méndez Alvaro 44, Madrid, 28045, Spain Departament de Géologia, Facultat de Ciències, Universitat Autònoma de Barcelona, Bellaterra, Barcelona, 08193, Spain Centre de Recherches Pétrographiques et Géochimiques, UMR7358, 15 rue Notre Dame des Pauvres, Vandoeuvre-lès-Nancy Cédex, F-54 501, France Université de Lorraine, CNRS, CREGU, GeoRessources UMR 7359, BP 70239, Vandoeuvre-lès-Nancy, F-54506, France Centro de Investigación y de Estudios Avanzados del Instituto Politecnico Nacional, Unidad Querétaro, Apartado Postal 1-798, Querétaro, Qro 76001, Mexico Cited By :2 Export Date: 12 September 2021 Correspondence Address: Levresse, G.; Programa de Geofluidos, AP 1-253, Mexico; email: glevresse@geociencias.unam.mx Funding details: IN100707, IN109410-3 Funding details: Consejo Nacional de Ciencia y Tecnología, CONACYT, 81584 Funding text 1: Special thanks to Marina Vega, Juan Tomas Vasquez Perez and Teresa Soledad Medina Malagón for their assistance at the CGEO laboratory. This study was financed by UNAM-PAPIIT projects IN100707 , IN109410-3 and CONACYT project 81584 . AB - The fluid history of "diamond" quartz crystals from Caravia-Berbes Fluorite district is intimately related with episodes of maturation and migration of hydrocarbons within the Asturian basin, probably linked to the structural activation of a Mesozoic rift system. These "diamond" quartz record the migration of hydrothermal silica-rich brines and associated hydrocarbons that recorded a temperature increase (outlined by fluid inclusion studies) from similar to 90 to similar to 140 degrees C. This gradient is also recorded by a change in the organic matter species trapped in quartz, from bitumen located in the inner quartz growth zones to liquid hydrocarbons trapped within the outer quartz overgrowths. Secondary ion mass spectrometer (SIMS) oxygen isotope microanalyses allowed to differentiate two delta O-18(H2O) values corresponding to the oil-dominated zone (core) and the water-dominated zone (outer growth zone). The heavier delta O-18(H2O) values in the water-dominated zone do not only record a higher temperature of formation, but also an increase in the delta O-18(H2O) of the parental fluid. Isotopic compositions of diamond quartz suggest a heterogeneous source of surficial fluids and formation-waters expelled from clays tones.Within the basin history, the diamond quartz precipitation took place during early Jurassic to Eocene subsidence periods. Pressure Temperature and composition (PTX) and delta O-18(H2O) characteristics point out a probable relationship with Albian diagenetic events reported in Cantabrian and north Pyrenean basins. LA - English DB - MTMT ER - TY - THES AU - Li, Ke TI - Geochemical Development of the Altered Horizon along the Great Unconformity in Gallinas Canyon, New Mexico, USA PY - 2019 SN - 9781085748117 UR - https://m2.mtmt.hu/api/publication/34621507 ID - 34621507 LA - English DB - MTMT ER - TY - JOUR AU - Volk, Herbert AU - George, Simon C. TI - Using petroleum inclusions to trace petroleum systems - A review JF - ORGANIC GEOCHEMISTRY J2 - ORG GEOCHEM VL - 129 PY - 2019 SP - 99 EP - 123 PG - 25 SN - 0146-6380 DO - 10.1016/j.orggeochem.2019.01.012 UR - https://m2.mtmt.hu/api/publication/30914074 ID - 30914074 N1 - Funding Agency and Grant Number: ARC (Australia)Australian Research Council [DP0556493, DP130102547]; Agouron Institute Research Grant for 2010-2013 (USA); Macquarie University; CSIROCommonwealth Scientific & Industrial Research Organisation (CSIRO); 2018 ARC LIEF grant [LE180100160] Funding text: We thank our many collaborators and colleagues who have worked with us over more than 20 years in developing these petroleum inclusion techniques and applications, and who have provided extensive advice and experience. These include Manzur Ahmed, Julien Bourdet, Peter Eadington, David Fuentes, Se Gong, Richard Kempton, Frank Krieger, Mark Lisk and Keyu Liu who work/worked at CSIRO, and Tim Leefmann, Kaikai Li, Guoyan Mu, Carl Peters and Hongwei Ping who worked or studied at Macquarie University. Other collaborators and colleagues have been Chris Boreham, Oliver Burde, Adriana Dutkiewicz, Dianne Edwards, Keith Hall, Brian Horsfield, John Kennard, Franz Leistner, Ulli Mann, John Ridley, Sandra Siljestrom, Roger Summons, Feiyu Wang and Ningning Zhong. Many studies would not have been possible without financial backing from the petroleum industry, for which we are very grateful. SCG acknowledges the support of ARC Discovery project grants DP0556493 and DP130102547 (Australia), an Agouron Institute Research Grant for 2010-2013 (USA), numerous internal Macquarie University grants, CSIRO funding of analytical equipment, and a 2018 ARC LIEF grant (LE180100160 "Femtosecond laser micropyrolysis gas chromatograph-mass spectrometer"), which will enable the continuation of parts of this work. HV thanks colleagues at BP for stimulating discussions and support to write this review. The opinions presented in this review are those of the authors only and do not in any way represent the view of BP Exploration Operating Company Ltd or Macquarie University. We thank the two anonymous journal reviewers for their helpful comments that improved the manuscript, and Andrew Murray (AE), Erdem Idiz (Editor-in-Chief) and Tim Horscroft (Review Papers Coordinator) for their support and advice throughout the publication process. Cited By :19 Export Date: 12 February 2021 CODEN: ORGED Correspondence Address: Volk, H.; BP Exploration Operating Company Ltd, Chertsey Road, United Kingdom; email: Herbert.Volk@uk.bp.com Funding details: Commonwealth Scientific and Industrial Research Organisation, CSIRO, LE180100160 Funding details: Macquarie University Funding details: Appalachian Regional Commission, ARC, DP0556493, DP130102547 Funding details: Agouron Institute Funding text 1: We thank our many collaborators and colleagues who have worked with us over more than 20 years in developing these petroleum inclusion techniques and applications, and who have provided extensive advice and experience. These include Manzur Ahmed, Julien Bourdet, Peter Eadington, David Fuentes, Se Gong, Richard Kempton, Frank Krieger, Mark Lisk and Keyu Liu who work/worked at CSIRO, and Tim Leefmann, Kaikai Li, Guoyan Mu, Carl Peters and Hongwei Ping who worked or studied at Macquarie University. Other collaborators and colleagues have been Chris Boreham, Oliver Burde, Adriana Dutkiewicz, Dianne Edwards, Keith Hall, Brian Horsfield, John Kennard, Franz Leistner, Ulli Mann, John Ridley, Sandra Siljeström, Roger Summons, Feiyu Wang and Ningning Zhong. Many studies would not have been possible without financial backing from the petroleum industry, for which we are very grateful. SCG acknowledges the support of ARC Discovery project grants DP0556493 and DP130102547 (Australia) , an Agouron Institute Research Grant for 2010–2013 (USA), numerous internal Macquarie University grants, CSIRO funding of analytical equipment, and a 2018 ARC LIEF grant (LE180100160 “Femtosecond laser micropyrolysis gas chromatograph-mass spectrometer”), which will enable the continuation of parts of this work. HV thanks colleagues at BP for stimulating discussions and support to write this review. The opinions presented in this review are those of the authors only and do not in any way represent the view of BP Exploration Operating Company Ltd or Macquarie University. We thank the two anonymous journal reviewers for their helpful comments that improved the manuscript, and Andrew Murray (AE), Erdem Idiz (Editor-in-Chief) and Tim Horscroft (Review Papers Coordinator) for their support and advice throughout the publication process. Cited By :24 Export Date: 12 September 2021 CODEN: ORGED Correspondence Address: Volk, H.; BP Exploration Operating Company Ltd, Chertsey Road, United Kingdom; email: Herbert.Volk@uk.bp.com Funding details: Agouron Institute Funding details: Australian Research Council, ARC, DP0556493, DP130102547 Funding details: Commonwealth Scientific and Industrial Research Organisation, CSIRO, LE180100160 Funding details: Macquarie University Funding text 1: We thank our many collaborators and colleagues who have worked with us over more than 20 years in developing these petroleum inclusion techniques and applications, and who have provided extensive advice and experience. These include Manzur Ahmed, Julien Bourdet, Peter Eadington, David Fuentes, Se Gong, Richard Kempton, Frank Krieger, Mark Lisk and Keyu Liu who work/worked at CSIRO, and Tim Leefmann, Kaikai Li, Guoyan Mu, Carl Peters and Hongwei Ping who worked or studied at Macquarie University. Other collaborators and colleagues have been Chris Boreham, Oliver Burde, Adriana Dutkiewicz, Dianne Edwards, Keith Hall, Brian Horsfield, John Kennard, Franz Leistner, Ulli Mann, John Ridley, Sandra Siljeström, Roger Summons, Feiyu Wang and Ningning Zhong. Many studies would not have been possible without financial backing from the petroleum industry, for which we are very grateful. SCG acknowledges the support of ARC Discovery project grants DP0556493 and DP130102547 (Australia) , an Agouron Institute Research Grant for 2010–2013 (USA), numerous internal Macquarie University grants, CSIRO funding of analytical equipment, and a 2018 ARC LIEF grant (LE180100160 “Femtosecond laser micropyrolysis gas chromatograph-mass spectrometer”), which will enable the continuation of parts of this work. HV thanks colleagues at BP for stimulating discussions and support to write this review. The opinions presented in this review are those of the authors only and do not in any way represent the view of BP Exploration Operating Company Ltd or Macquarie University. We thank the two anonymous journal reviewers for their helpful comments that improved the manuscript, and Andrew Murray (AE), Erdem Idiz (Editor-in-Chief) and Tim Horscroft (Review Papers Coordinator) for their support and advice throughout the publication process. AB - Petroleum-bearing fluid inclusions are small encapsulations of oil and gas that offer an invaluable opportunity to better constrain the evolution of petroleum systems. Insights into palaeo fluid compositions complement observations on present day fluid compositions, which represent only the end-point of complex cumulative processes throughout basin history. In this contribution, we review a wide range of approaches used to extract geochemical information from petroleum inclusions, and how these can be used to better constrain petroleum systems. These techniques can be grouped into optical, spectrographic and thermometric non-destructive methods, or destructive chemical analyses of bulk samples or individual inclusions.Typically optical methods documenting the distribution and visual properties of petroleum inclusions are used to provide petrographic context for subsequent specialised geochemical analyses of petroleum inclusions. Additional non-destructive techniques such as Raman spectroscopy can then be applied to provide some further insights into the composition of the trapped fluids, although the complex nature of petroleum generally requires direct access to the fluid for a more complete understanding of geochemical aspects. A variety of destructive techniques have been developed, initially to analyse bulk samples released by mechanical crushing and more recently through ablation type techniques that allow the composition of individual inclusions to be characterised.Screening geochemical techniques that utilise mechanical crushing of bulk samples to analyse petroleum inclusions using mass spectrometry without prior chromatographic separation have become routine analyses. Other geochemical techniques more geared towards detailed molecular information such as biomarkers utilise chromatographic separation prior to mass spectrometry. Evaluation of the isotopic composition of petroleum inclusions is also possible for both bulk samples and compound specific analyses.The use of lasers to open individual inclusions allows the released contents to be analysed by thermal extraction-gas chromatography-mass spectrometry (GC-MS), or mass spectrometric mapping of minerals using Time-of-Flight Secondary Ion Mass Spectrometry (ToF-SIMS), a surface-sensitive analytical method that uses ion beams to ablate into minerals.The continued evolution of techniques to analyse the incredibly small volume of hydrocarbons trapped within fluid inclusions has progressed to a point where there is little that can be done to evaluate a live oil or gas sample that cannot be achieved for a fluid inclusion sample. The full power for tracing petroleum systems is, however, only realised where there is an effective integration of fluid inclusion data with a more conventional approach to petroleum systems analysis. (C) 2019 Elsevier Ltd. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Garaguly, István AU - Raucsikné Varga, Andrea Beáta AU - Raucsik, Béla AU - Schubert, Félix AU - Czuppon, György AU - Frei, R TI - Pervasive early diagenetic dolomitization, subsequent hydrothermal alteration, and late stage hydrocarbon accumulation in a Middle Triassic carbonate sequence (Szeged Basin, SE Hungary) JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 98 PY - 2018 SP - 270 EP - 290 PG - 21 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2018.07.024 UR - https://m2.mtmt.hu/api/publication/3399845 ID - 3399845 N1 - Funding Agency and Grant Number: National Research, Development and Innovation Fund of Hungary [K 108375] Funding text: This research was supported by the National Research, Development and Innovation Fund of Hungary (project no. K 108375). The authors would like to thank MOL Plc for providing the core material that were essential for this research. We would like to thank Dr. Fadi H. Nader and the anonymous referee for their suggestions and comments that improve our manuscript, as well as Associated Editor Dr. Ihsan Al-Aasm for the editorial work. Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem utca 2-6, Szeged, 6702, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary Department of Geosciences and Natural Resource Management, University of Copenhagen, ØsterVoldgade10, Copenhagen, 1350, Denmark Nordic Center for Earth Evolution (NordCEE), Copenhagen, Denmark Cited By :15 Export Date: 12 September 2021 Correspondence Address: Garaguly, I.; Department of Mineralogy, Egyetem utca 2-6, Hungary; email: garagulyistvan@gmail.com Funding text 1: This research was supported by the National Research, Development and Innovation Fund of Hungary (project no. K 108375 ). The authors would like to thank MOL Plc for providing the core material that were essential for this research. We would like to thank Dr. Fadi H. Nader and the anonymous referee for their suggestions and comments that improve our manuscript, as well as Associated Editor Dr. Ihsan Al-Aasm for the editorial work. LA - English DB - MTMT ER - TY - JOUR AU - Jiang, Y. AU - Zhang, W. AU - Liu, H. AU - Yang, D. AU - Wang, X. TI - Properties of fluid inclusions and periods of hydrocarbon accumulation in Paleogene reservoirs in Raoyang Depression JF - ZHONGGUO SHIYOU DAXUE XUEBAO (ZIRAN KEXUE BAN) / JOURNAL OF CHINA UNIVERSITY OF PETROLEUM (EDITION OF NATURAL SCIENCE) J2 - J CHINA UNIV PETROLEUM (ED NATUR SCI) VL - 42 PY - 2018 IS - 4 SP - 23 EP - 33 PG - 11 SN - 1673-5005 DO - 10.3969/j.issn.1673-5005.2018.04.003 UR - https://m2.mtmt.hu/api/publication/31867557 ID - 31867557 N1 - School of Geosciences in China University of Petroleum(East China), Qingdao, 266580, China Research Institute of Petroleum Exploration & Development, Huabei Oilfield Company, PetroChina, Renqiu, 062552, China Cited By :8 Export Date: 12 February 2021 Correspondence Address: Jiang, Y.; School of Geosciences in China University of Petroleum(East China)China; email: jiangyl@upc.edu.cn School of Geosciences in China University of Petroleum(East China), Qingdao, 266580, China Research Institute of Petroleum Exploration & Development, Huabei Oilfield Company, PetroChina, Renqiu, 062552, China Cited By :9 Export Date: 12 September 2021 Correspondence Address: Jiang, Y.; School of Geosciences in China University of Petroleum(East China)China; email: jiangyl@upc.edu.cn AB - Taking an example of Paleogene reservoirs in Raoyang Depression,a detailed study was carried out to determine properties of fluid inclusions through a combination of microscopic examination and micro-thermometric techniques. The hydrocarbon accumulation periods were defined by analyzing the hydrocarbon-generating history of source rocks. The results indicate that the hydrocarbon inclusions can be divided into two phases. The first phase is located in the carbonate cements and the fractures within quartz grains with characteristic yellow fluorescence, high salinity and high density. The homogenization temperature of brine inclusions is from 90 ℃ to 100 ℃. The second phase is located in the dissolution fractures of feldspar and fractures through quartz grains with blue-green fluorescence, low salinity and low density.The homogenization temperature is mainly from 120 ℃ to 140 ℃.There are two major hydrocarbon-generating stages: the Dongying deposition period and the late Guantao deposition period to the Minghuazhen deposition period.The Minghuazhen deposition period is the major stage.A two-period hydrocarbon accumulation is identified in Paleogene reservoirs. The first period is from the late Dongying deposition period to the early uplift stage, and the second is from the late Guantao deposition period to the Minghuazhen deposition period. Controlled by the thermal evolution and hydrocarbon-generating history of source rocks, the accumulation periods of different parts and layers are different. Petroleum reservoirs generated in the early period are mainly distributed in the source rock layers in the center of hydrocarbon-generating sags. Reservoirs generated in the second period cover all the area which is the main accumulation period.The upper layers are characterized with late accumulation period, while the lower with two periods. © 2018, Periodical Office of China University of Petroleum. All right reserved. LA - Chinese DB - MTMT ER - TY - JOUR AU - Rudmin, Maxim AU - Roberts, Andrew P AU - Horng, Chorng-Shern AU - Mazurov, Aleksey AU - Savinova, Olesya AU - Ruban, Aleksey AU - Kashapov, Roman AU - Veklich, Maxim TI - Ferrimagnetic Iron Sulfide Formation and Methane Venting Across the Paleocene-Eocene Thermal Maximum in Shallow Marine Sediments, Ancient West Siberian Sea JF - GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS J2 - GEOCHEM GEOPHY GEOSY VL - 19 PY - 2018 IS - 1 SP - 21 EP - 42 PG - 22 SN - 1525-2027 DO - 10.1002/2017GC007208 UR - https://m2.mtmt.hu/api/publication/27316426 ID - 27316426 N1 - Funding Agency and Grant Number: Russian Foundation of Basic ResearchRussian Foundation for Basic Research (RFBR) [18-35-00022, 16-45-700090]; Australian Research CouncilAustralian Research Council [DP140104544] Funding text: This study was supported by the Russian Foundation of Basic Research (grants 18-35-00022 and 16-45-700090) and by the Australian Research Council (grant DP140104544). Laboratory investigations were carried out at Tomsk Polytechnic University within the framework of a Tomsk Polytechnic University Competitiveness Enhancement Program grant. We thank N. Guseva, A. Khvashchevskaya, and I. Mazurova (Tomsk Polytechnic University) for assistance with geochemical analyses, and the Tomsk Oil and Gas Research and Design Institute for use of their mass spectrometer. We also thank the editor Y. Yokoyama, an anonymous reviewer, and Myriam Kars for their constructive reviews, which led to improvement of the manuscript. Supporting information is available from data repository Figshare (https://doi.org/10.6084/m9.figshare.5596858.v1). Department of Geology and Mineral Exploration, Institute of Natural Resources, Tomsk Polytechnic University, Tomsk, Russian Federation Research School of Earth Sciences, The Australian National University, Canberra, ACT, Australia Institute of Earth Sciences, Academia Sinica, Nangang, Taipei, Taiwan Tomsk Oil and Gas Research and Design Institute, Tomsk, Russian Federation Cited By :11 Export Date: 12 February 2021 Correspondence Address: Rudmin, M.; Department of Geology and Mineral Exploration, Russian Federation; email: rudminma@tpu.ru Funding details: Australian Research Council, ARC, DP140104544 Funding details: Russian Foundation for Basic Research, RFBR, 16–45- 700090, 18–35-00022 Funding text 1: This study was supported by the Russian Foundation of Basic Research (grants 18–35-00022 and 16–45- 700090) and by the Australian Research Council (grant DP140104544). Laboratory investigations were carried out at Tomsk Polytechnic University within the framework of a Tomsk Polytechnic University Competitiveness Enhancement Program grant. We thank N. Guseva, A. Khvashchevskaya, and I. Mazurova (Tomsk Polytechnic University) for assistance with geochemical analyses, and the Tomsk Oil and Gas Research and Design Institute for use of their mass spectrometer. We also thank the editor Y. Yokoyama, an anonymous reviewer, and Myriam Kars for their constructive reviews, which led to improvement of the manuscript. Supporting information is available from data repository Figshare (https://doi.org/10. 6084/m9.figshare.5596858.v1). Department of Geology and Mineral Exploration, Institute of Natural Resources, Tomsk Polytechnic University, Tomsk, Russian Federation Research School of Earth Sciences, The Australian National University, Canberra, ACT, Australia Institute of Earth Sciences, Academia Sinica, Nangang, Taipei, Taiwan Tomsk Oil and Gas Research and Design Institute, Tomsk, Russian Federation Cited By :13 Export Date: 12 September 2021 Correspondence Address: Rudmin, M.; Department of Geology and Mineral Exploration, Russian Federation; email: rudminma@tpu.ru Funding details: Australian Research Council, ARC, DP140104544 Funding details: Russian Foundation for Basic Research, RFBR, 16–45- 700090, 18–35-00022 Funding text 1: This study was supported by the Russian Foundation of Basic Research (grants 18–35-00022 and 16–45- 700090) and by the Australian Research Council (grant DP140104544). Laboratory investigations were carried out at Tomsk Polytechnic University within the framework of a Tomsk Polytechnic University Competitiveness Enhancement Program grant. We thank N. Guseva, A. Khvashchevskaya, and I. Mazurova (Tomsk Polytechnic University) for assistance with geochemical analyses, and the Tomsk Oil and Gas Research and Design Institute for use of their mass spectrometer. We also thank the editor Y. Yokoyama, an anonymous reviewer, and Myriam Kars for their constructive reviews, which led to improvement of the manuscript. Supporting information is available from data repository Figshare (https://doi.org/10. 6084/m9.figshare.5596858.v1). LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Schubert, Félix TI - Evolution of the arc-derived orthogneiss recorded in exotic xenoliths of the Koros Complex (Tisza Megaunit, SE Hungary) JF - JOURNAL OF GEOSCIENCES J2 - J GEOSCI VL - 63 PY - 2018 IS - 1 SP - 21 EP - 46 PG - 26 SN - 1802-6222 DO - 10.3190/jgeosci.253 UR - https://m2.mtmt.hu/api/publication/27569302 ID - 27569302 N1 - Funding Agency and Grant Number: Schweizerische NationalfondsSwiss National Science Foundation (SNSF) [21-26579.89] Funding text: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Zavada, Martin Racek and an anonymous reviewer are thanked. P. Hasalova is acknowledged for her editorial work on the manuscript. Cited By :1 Export Date: 11 February 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Egyetem str. 2-6, Hungary; email: mtoth@geo.u-szeged.hu Funding details: Universität Bern, Ub, 21-26579.89 Funding text 1: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Funding text 2: Acknowledgements. The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Cited By :1 Export Date: 12 February 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Egyetem str. 2-6, Hungary; email: mtoth@geo.u-szeged.hu Funding details: Universität Bern, Ub, 21-26579.89 Funding text 1: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Funding text 2: Acknowledgements. The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Cited By :3 Export Date: 12 September 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Egyetem str. 2-6, Hungary; email: mtoth@geo.u-szeged.hu Funding details: Universität Bern, Ub, 21-26579.89 Funding text 1: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Funding text 2: Acknowledgements. The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Vass, I AU - M. Tóth, Tivadar AU - Szanyi, János AU - Kovács, Balázs TI - Hybrid numerical modelling of fluid and heat transport between the overpressured and gravitational flow systems of the Pannonian Basin JF - GEOTHERMICS J2 - GEOTHERMICS VL - 72 PY - 2018 SP - 268 EP - 276 PG - 9 SN - 0375-6505 DO - 10.1016/j.geothermics.2017.11.013 UR - https://m2.mtmt.hu/api/publication/3331146 ID - 3331146 N1 - MOL Plc., Október huszonharmadika str. 18., Budapest, 1117, Hungary Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem street 2., Szeged, 6722, Hungary Institute of Environmental Management, University of Miskolc, Miskolc-Egyetemváros, 3515, Hungary Cited By :1 Export Date: 18 December 2018 CODEN: GTMCA Correspondence Address: Vass, I.; MOL Plc., Október huszonharmadika str. 18., Hungary; email: ivass.geo@gmail.com MOL Plc., Október huszonharmadika str. 18., Budapest, 1117, Hungary Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem street 2., Szeged, 6722, Hungary Institute of Environmental Management, University of Miskolc, Miskolc-Egyetemváros, 3515, Hungary Cited By :5 Export Date: 11 February 2021 CODEN: GTMCA Correspondence Address: Vass, I.; MOL Plc., Október huszonharmadika str. 18., Hungary; email: ivass.geo@gmail.com MOL Plc., Október huszonharmadika str. 18., Budapest, 1117, Hungary Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem street 2., Szeged, 6722, Hungary Institute of Environmental Management, University of Miskolc, Miskolc-Egyetemváros, 3515, Hungary Cited By :5 Export Date: 12 February 2021 CODEN: GTMCA Correspondence Address: Vass, I.; MOL Plc., Október huszonharmadika str. 18., Hungary; email: ivass.geo@gmail.com MOL Plc., Október huszonharmadika str. 18., Budapest, 1117, Hungary Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem street 2., Szeged, 6722, Hungary Institute of Environmental Management, University of Miskolc, Miskolc-Egyetemváros, 3515, Hungary Cited By :7 Export Date: 12 September 2021 CODEN: GTMCA Correspondence Address: Vass, I.; MOL Plc., Október huszonharmadika str. 18., Hungary; email: ivass.geo@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Wu, Jia AU - Ni, Zhiyong AU - Wang, Shixia AU - Zheng, Haifei TI - An in-situ Raman study on pristane at high pressure and ambient temperature JF - SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY J2 - SPECTROCHIM ACTA A VL - 189 PY - 2018 SP - 215 EP - 220 PG - 6 SN - 1386-1425 DO - 10.1016/j.saa.2017.07.026 UR - https://m2.mtmt.hu/api/publication/27316425 ID - 27316425 N1 - Funding Agency and Grant Number: National Natural Science Foundation of ChinaNational Natural Science Foundation of China (NSFC) [41403049, 41103002]; Science Foundation of China University of Petroleum, Beijing [2462014YJRC002]; Foundation of State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum, Beijing [PRP/open-1311] Funding text: We would like to thank Jingqiu Ren (Peking University) for his assistance in the Raman measurements. This work was supported by National Natural Science Foundation of China (No. 41403049, and 41103002), Science Foundation of China University of Petroleum, Beijing (No. 2462014YJRC002), and the Foundation of State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum, Beijing (No. PRP/open-1311). State Key Laboratory of Petroleum Resources and Engineering − College of Geoscience, China University of Petroleum, Beijing, 102249, China College of Science, University of Shanghai for Science and Technology, Shanghai, 200093, China Key Laboratory of Orogenic Belts and Crustal Evolution, Department of Geology, Peking University, Beijing, 100871, China Export Date: 12 February 2021 CODEN: SAMCA Correspondence Address: Wu, J.; State Key Laboratory of Petroleum Resources and Engineering − College of Geoscience, China; email: jia.wu@cup.edu.cn Funding details: China University of Petroleum, Beijing Funding details: China University of Petroleum, Beijing, PRP/open-1311 Funding details: China University of Petroleum, Beijing Funding details: China University of Petroleum, Beijing Funding details: Peking University Funding details: State Key Laboratory of Agrobiotechnology, China Agricultural University Funding details: Beijing Nova Program, 2462014YJRC002 Funding details: National Natural Science Foundation of China, 41403049, 41103002 Funding text 1: We would like to thank Jingqiu Ren (Peking University) for his assistance in the Raman measurements. This work was supported by National Natural Science Foundation of China (No. 41403049 , and 41103002 ), Science Foundation of China University of Petroleum, Beijing (No. 2462014YJRC002 ), and the Foundation of State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum, Beijing (No. PRP/open-1311 ). State Key Laboratory of Petroleum Resources and Engineering − College of Geoscience, China University of Petroleum, Beijing, 102249, China College of Science, University of Shanghai for Science and Technology, Shanghai, 200093, China Key Laboratory of Orogenic Belts and Crustal Evolution, Department of Geology, Peking University, Beijing, 100871, China Export Date: 12 September 2021 CODEN: SAMCA Correspondence Address: Wu, J.; State Key Laboratory of Petroleum Resources and Engineering − College of Geoscience, China; email: jia.wu@cup.edu.cn Funding details: National Natural Science Foundation of China, 41103002, 41403049 Funding details: China University of Petroleum, Beijing, PRP/open-1311 Funding details: State Key Laboratory of Agrobiotechnology, China Agricultural University Funding details: Beijing Nova Program, 2462014YJRC002 Funding details: Peking University Funding text 1: We would like to thank Jingqiu Ren (Peking University) for his assistance in the Raman measurements. This work was supported by National Natural Science Foundation of China (No. 41403049 , and 41103002 ), Science Foundation of China University of Petroleum, Beijing (No. 2462014YJRC002 ), and the Foundation of State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum, Beijing (No. PRP/open-1311 ). LA - English DB - MTMT ER - TY - JOUR AU - Berkesi, Márta AU - Káldos, Réka AU - Park, M AU - Szabó, Csaba AU - Váczi, Tamás AU - Török, Kálmán AU - Németh, Bianka AU - Czuppon, György TI - Detection of small amounts of N2 in CO2-rich high-density fluid inclusions from mantle xenoliths JF - EUROPEAN JOURNAL OF MINERALOGY J2 - EUR J MINERAL VL - 29 PY - 2017 IS - 3 SP - 423 EP - 431 PG - 9 SN - 0935-1221 DO - 10.1127/ejm/2017/0029-2615 UR - https://m2.mtmt.hu/api/publication/3158610 ID - 3158610 LA - English DB - MTMT ER - TY - JOUR AU - Szabó, B AU - Schubert, Félix AU - M. Tóth, Tivadar AU - Steinbach, Gábor TI - Palaeofluid evolution in a fractured basalt hosted reservoir in the Üllés-Ruzsa-Bordány area, southern sector of the Pannonian Basin JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 69 PY - 2016 IS - 3 SP - 281 EP - 293 PG - 13 SN - 1330-030X DO - 10.4154/gc.2016.25 UR - https://m2.mtmt.hu/api/publication/3126648 ID - 3126648 N1 - Funding Agency and Grant Number: MOL Ltd.; Hungarian National Scientific Research Fund (OTKA)Orszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [K 108375] Funding text: The authors thank MOL Ltd. for their financial support of the project. Special thanks go to Robert GYURCSANYI (Budapest University of Technology and Ecomics) for his help with UV fluorescent micro-spectroscopy and Andras SZABO (Budapest University of Technology and Ecomics) and Eric Le MENN (University of Nantes) for their help in the Raman micro-spectrometric measurements. The research was supported by Hungarian National Scientific Research Fund (OTKA, K 108375). Cited By :7 Export Date: 12 February 2021 Correspondence Address: Szabo, B.; Exploration and Production MOL Plc.Hungary; email: barbokster@gmail.com Cited By :7 Export Date: 12 September 2021 Correspondence Address: Szabo, B.; Exploration and Production MOL Plc.Hungary; email: barbokster@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Molnár, L AU - M. Tóth, Tivadar AU - Schubert, Félix TI - Structural controls on petroleum migration and entrapment within the faulted basement blocks of Szeghalom Dome (Pannonian Basin, SE Hungary) JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 68 PY - 2015 IS - 3 SP - 247 EP - 259 PG - 14 SN - 1330-030X DO - 10.4154/gc.2015.19 UR - https://m2.mtmt.hu/api/publication/2949635 ID - 2949635 N1 - Funding Agency and Grant Number: research Balazs KISS (MOL) Funding text: We thank MOL Hungarian Oil and Gas Company for providing the samples, datasets and the financial support of this research Balazs KISS (MOL) is thanked for the fruitful discussions about the behaviour of the Szeghalom reservoir. Reviews by Istvan BERCZI and Gyula MAROS have significantly improved the manuscript, and are much appreciated. English was corrected by American Journal Experts. Cited By :5 Export Date: 11 February 2021 Cited By :5 Export Date: 12 February 2021 Cited By :6 Export Date: 12 September 2021 LA - English DB - MTMT ER - TY - THES AU - Pinke, Zsolt László TI - Alkalmazkodás és felemelkedés – modernizáció és leszakadás. Kis jégkorszaki kihívások és társadalmi válaszok a Tiszántúlon TS - Kis jégkorszaki kihívások és társadalmi válaszok a Tiszántúlon PB - Pécsi Tudományegyetem PY - 2015 SP - 332 UR - https://m2.mtmt.hu/api/publication/3020109 ID - 3020109 N1 - Megjegyzés-24933529 117., 366. sz. jegyzet Megjegyzés-24933530 282. Megjegyzés-25207233 259. p. 746. lj. Megjegyzés-27674501 29. old. 65. jegyzet LA - Hungarian DB - MTMT ER - TY - JOUR AU - Zhang, Junwu AU - Zou, Huayao AU - Li, Pingping AU - Fu, Xiaoyue AU - Wang, Wei TI - 含烃盐水包裹体 PVT 模拟新方法及其 在气藏古压力恢复中的应用 [A new PVT simulation method for hydrocarbon-containing inclusions and its application to reconstructing paleo-pressure of gas reservoirs] JF - Petroleum Geology & Experiment J2 - Petroleum Geology & Experiment VL - 37 PY - 2015 IS - 1 SP - 102 EP - 108 PG - 7 SN - 1001-6112 DO - 10.7603/s40972-015-0017-3 UR - https://m2.mtmt.hu/api/publication/24737105 ID - 24737105 LA - Chinese DB - MTMT ER - TY - JOUR AU - Mark, A Evans AU - Amanda, DeLisle AU - Jeremy, Leo AU - Christopher, J Lafonte TI - Deformation conditions for fracturing in the Middle Devonian sequence of the central Appalachians during the Late Paleozoic Alleghenian orogeny JF - AAPG BULLETIN J2 - AAPG BULL VL - 98 PY - 2014 IS - 11 SP - 2263 SN - 0149-1423 DO - 10.1306/07221413135 UR - https://m2.mtmt.hu/api/publication/24832643 ID - 24832643 N1 - Funding Agency and Grant Number: American Chemical SocietyAmerican Chemical Society; Appalachian Basin Black Shale Group, a Penn State industry consortium Funding text: The authors thank the Petroleum Research Fund of the American Chemical Society for funding. In addition, we also thank Terry Engelder for access to and sampling of the shallow cores, and the Appalachian Basin Black Shale Group, a Penn State industry consortium, for partial funding. Mike Jercinovic and the University of Massachusetts deserve thanks for use of the SEM-CL. We also thank David Haddad and Steve Laubach for thoughtful reviews of the manuscript. Central Connecticut State University, Department of Physics and Earth Science, New Britain, CT 06050, United States Carmin International, Inc., Olathe, KS 66062-3426, United States Department of Geology, Bowling Green State University, Bowling Green, OH 45403-0211, United States Cited By :17 Export Date: 12 February 2021 CODEN: AABUD Central Connecticut State University, Department of Physics and Earth Science, New Britain, CT 06050, United States Carmin International, Inc., Olathe, KS 66062-3426, United States Department of Geology, Bowling Green State University, Bowling Green, OH 45403-0211, United States Cited By :19 Export Date: 12 September 2021 CODEN: AABUD LA - English DB - MTMT ER - TY - JOUR AU - Molnár, László AU - M. Tóth, Tivadar AU - Schubert, Félix TI - Statistical characterization of brittle and semi-brittle fault rocks: a clast geometry approach JF - ACTA GEODAETICA ET GEOPHYSICA J2 - ACTA GEOD GEOPHYS VL - 49 PY - 2014 IS - 4 SP - 527 EP - 550 PG - 24 SN - 2213-5812 DO - 10.1007/s40328-014-0067-3 UR - https://m2.mtmt.hu/api/publication/2783510 ID - 2783510 N1 - Funding Agency and Grant Number: MOL Hungarian Oil and Gas Company Funding text: We thank MOL Hungarian Oil and Gas Company for providing the samples and the financial support of this research. We are grateful to Gyula Maros (Hungarian Geological and Geophysical Institute) for his help in the use of ImaGeo corescanner. English was corrected by Proof-Reading-Service.com. Cited By :2 Export Date: 12 February 2021 Correspondence Address: Molnár, L.; Department of Mineralogy, Egyetem utca 2, Hungary Funding text 1: Acknowledgments We thank MOL Hungarian Oil and Gas Company for providing the samples and the financial support of this research. We are grateful to Gyula Maros (Hungarian Geological and Geophysical Institute) for his help in the use of ImaGeo corescanner. English was corrected by Proof-Reading-Service.com. Cited By :2 Export Date: 12 September 2021 Correspondence Address: Molnár, L.; Department of Mineralogy, Egyetem utca 2, Hungary Funding text 1: Acknowledgments We thank MOL Hungarian Oil and Gas Company for providing the samples and the financial support of this research. We are grateful to Gyula Maros (Hungarian Geological and Geophysical Institute) for his help in the use of ImaGeo corescanner. English was corrected by Proof-Reading-Service.com. LA - English DB - MTMT ER - TY - JOUR AU - Zhang, Q. AU - Zhu, X. AU - Steel, R. J. AU - Wang, G. AU - Ji, H. TI - Fluid Inclusions and Their Application in Hydrocarbon History and Genesis JF - PETROLEUM SCIENCE AND TECHNOLOGY J2 - PETROL SCI TECHNOL VL - 32 PY - 2014 IS - 24 SP - 2911 EP - 2920 PG - 10 SN - 1091-6466 DO - 10.1080/10916466.2014.933976 UR - https://m2.mtmt.hu/api/publication/31857707 ID - 31857707 N1 - Funding Agency and Grant Number: Science Foundation of China University of Petroleum, Beijing [KYJJ2012-01-29]; National Nature Science Foundation of ChinaNational Natural Science Foundation of China (NSFC) [ZX20130157] Funding text: The authors acknowledge the assistance of Science Foundation of China University of Petroleum, Beijing (KYJJ2012-01-29) and National Nature Science Foundation of China (ZX20130157). State Key Laboratory of Petroleum Resource and Prospecting, College of Geosciences, China University of Petroleum, Beijing, 102249, China Department of Geological Sciences, University of Texas at Austin, Austin, TX, United States Cited By :1 Export Date: 12 February 2021 CODEN: PSTEF Correspondence Address: Zhang, Q.; State Key Laboratory of Petroleum Resource and Prospecting, China Funding details: China University of Petroleum, Beijing, CUPB, KYJJ2012-01-29 Funding details: ZX20130157 Funding text 1: The authors acknowledge the assistance of Science Foundation of China University of Petroleum, Beijing (KYJJ2012-01-29) and National Nature Science Foundation of China (ZX20130157). State Key Laboratory of Petroleum Resource and Prospecting, College of Geosciences, China University of Petroleum, Beijing, 102249, China Department of Geological Sciences, University of Texas at Austin, Austin, TX, United States Cited By :1 Export Date: 12 September 2021 CODEN: PSTEF Correspondence Address: Zhang, Q.; State Key Laboratory of Petroleum Resource and Prospecting, China Funding details: China University of Petroleum, Beijing, CUPB, KYJJ2012-01-29 Funding details: National Natural Science Foundation of China, NSFC, ZX20130157 Funding text 1: The authors acknowledge the assistance of Science Foundation of China University of Petroleum, Beijing (KYJJ2012-01-29) and National Nature Science Foundation of China (ZX20130157). AB - The fluid inclusions characteristics and pore fluid salinity of 56 samples from clastic reservoir of the Lower Cretaceous were analyzed in the Tanzhuang Sag. The authors also discuss the hydrocarbon charge history and the genesis of secondary pores in the Lower Cretaceous. The multipeak distribution of homogenous temperature of the brine inclusions showed that the inclusions captured should be multiperiod fluids at various depths. Comparison of the homogeneous temperature of brine inclusions with the temperature on the burial history curve suggested that the source rocks had entered the stage of large-scale hydrocarbon generation. However, only individual brine inclusions containing methane were found, and no oil-bearing inclusions were seen. The absence of oil-bearing inclusions indicated that no large-scale oil charges and limited favorable mature source rocks were present in the study area. The paleosalinity varied with depth and was divided into three zones, namely two low-value zones in the shallow and deep burial and one high-value zone in the medium burial. The secondary pores were relatively developed in the high-salinity fluid zone. Secondary pores are chiefly related to the inorganic acid associated with dehydration and mutual transformation of clay materials, and to the organic acid released from limited mature organic matter. LA - English DB - MTMT ER - TY - CHAP AU - Falcó, I.P.R. ED - Leo, M.L. Nollet ED - Leen, S. P. De Gelder TI - Petroleum Hydrocarbon Analysis T2 - Handbook of Water Analysis: Third Edition PB - CRC Press CY - Boca Raton, Florida SN - 9780429112775 T3 - Handb. of Water Analysis: Third Edition PY - 2013 SP - 845 EP - 868 PG - 24 DO - 10.1201/b15314-34 UR - https://m2.mtmt.hu/api/publication/33767201 ID - 33767201 AB - Petroleum is a word that comes from the Greek word petros (rock) and Latin word oleum or Greek elaion (oil), so petroleum means “rock oil.” Petroleum is the most important source of energy and one of the main chemical industries in the world, and it is expected to remain so over the next decades. Petroleum is a complex mixture of different organic compounds or hydrocarbons. These compounds are formed mainly from carbon and hydrogen elements with different length of chain or number of aromatic rings going from light gases to heavy residues. Other elements are present in lower proportion such as sulfur, oxygen, and nitrogen, or metals to a lower extent. Petroleum hydrocarbons, a term used to refer to crude oil and the rened products from it, are usually obtained from distillation of crude oil. The nal product composition depends on the crude oil source and the rening process used to produce it, so it varies, not only among the product types, but also within each product type. © 2014 by Taylor and Francis Group, LLC. LA - English DB - MTMT ER - TY - THES AU - István, Vass TI - Hydrodynamic and Heat Transport Modeling of Underground Fluid Reservoirs Based on a Complex Crack Network Analysis Method PY - 2013 SN - 9798381043129 UR - https://m2.mtmt.hu/api/publication/34621508 ID - 34621508 LA - English DB - MTMT ER - TY - JOUR AU - Fiser-Nagy, Ágnes AU - M. Tóth, Tivadar AU - Vásárhelyi, Balázs AU - Földes, Tamás TI - Integrated core study of a fractured metamorphic HC-reservoir; Kiskunhalas-NE, Pannonian Basin JF - ACTA GEODAETICA ET GEOPHYSICA J2 - ACTA GEOD GEOPHYS VL - 48 PY - 2013 IS - 1 SP - 53 EP - 75 PG - 23 SN - 2213-5812 DO - 10.1007/s40328-012-0008-y UR - https://m2.mtmt.hu/api/publication/2190426 ID - 2190426 N1 - Funding Agency and Grant Number: European UnionEuropean Union (EU); European Social FundEuropean Social Fund (ESF); [TAMOP-4.2.2/B-10/1-2010-0012] Funding text: We thank MOL Hungarian Oil and Gas Company for making the study of the samples and thin sections possible. Balazs Kiss is thanked for the fruitful discussions about the behaviour of the KIHANE reservoir. The publication is supported by the European Union and co-funded by the European Social Fund. Project title: "Broadening the knowledge base and supporting the long term professional sustainability of the Research University Centre of Excellence at the University of Szeged by ensuring the rising generation of excellent scientists". Project number: TAMOP-4.2.2/B-10/1-2010-0012. English was corrected by Proof-Reading-Service.com. Department of Mineralogy Geochemistry and Petrology, University of Szeged, P.O. Box 651, 6701 Szeged, Hungary Department of Structural Engineering, Pollack Mihály Faculty of Engineering, University of Pécs, Pécs, Hungary Institute of Diagnostic Imaging and Radiation Oncology, Kaposvár University, Kaposvár, Hungary Cited By :1 Export Date: 11 February 2021 Correspondence Address: Nagy, A.; Department of Mineralogy Geochemistry and Petrology, P.O. Box 651, 6701 Szeged, Hungary; email: agnes.nagy@geo.u-szeged.hu Funding details: European Social Fund, ESF Funding details: European Commission, EC Funding text 1: Acknowledgements We thank MOL Hungarian Oil and Gas Company for making the study of the samples and thin sections possible. Balázs Kiss is thanked for the fruitful discussions about the behaviour of the KIHA-NE reservoir. The publication is supported by the European Union and co-funded by the European Social Fund. Project title: “Broadening the knowledge base and supporting the long term professional sustainability of the Research University Centre of Excellence at the University of Szeged by ensuring the rising generation of excellent scientists”. Project number: TÁMOP-4.2.2/B-10/1-2010-0012. English was corrected by ProofReading-Service.com. Department of Mineralogy Geochemistry and Petrology, University of Szeged, P.O. Box 651, 6701 Szeged, Hungary Department of Structural Engineering, Pollack Mihály Faculty of Engineering, University of Pécs, Pécs, Hungary Institute of Diagnostic Imaging and Radiation Oncology, Kaposvár University, Kaposvár, Hungary Cited By :1 Export Date: 12 February 2021 Correspondence Address: Nagy, A.; Department of Mineralogy Geochemistry and Petrology, P.O. Box 651, 6701 Szeged, Hungary; email: agnes.nagy@geo.u-szeged.hu Funding details: European Social Fund, ESF Funding details: European Commission, EC Funding text 1: Acknowledgements We thank MOL Hungarian Oil and Gas Company for making the study of the samples and thin sections possible. Balázs Kiss is thanked for the fruitful discussions about the behaviour of the KIHA-NE reservoir. The publication is supported by the European Union and co-funded by the European Social Fund. Project title: “Broadening the knowledge base and supporting the long term professional sustainability of the Research University Centre of Excellence at the University of Szeged by ensuring the rising generation of excellent scientists”. Project number: TÁMOP-4.2.2/B-10/1-2010-0012. English was corrected by ProofReading-Service.com. Department of Mineralogy Geochemistry and Petrology, University of Szeged, P.O. Box 651, 6701 Szeged, Hungary Department of Structural Engineering, Pollack Mihály Faculty of Engineering, University of Pécs, Pécs, Hungary Institute of Diagnostic Imaging and Radiation Oncology, Kaposvár University, Kaposvár, Hungary Cited By :3 Export Date: 12 September 2021 Correspondence Address: Nagy, A.; Department of Mineralogy Geochemistry and Petrology, P.O. Box 651, 6701 Szeged, Hungary; email: agnes.nagy@geo.u-szeged.hu Funding details: European Commission, EC Funding details: European Social Fund, ESF Funding text 1: Acknowledgements We thank MOL Hungarian Oil and Gas Company for making the study of the samples and thin sections possible. Balázs Kiss is thanked for the fruitful discussions about the behaviour of the KIHA-NE reservoir. The publication is supported by the European Union and co-funded by the European Social Fund. Project title: “Broadening the knowledge base and supporting the long term professional sustainability of the Research University Centre of Excellence at the University of Szeged by ensuring the rising generation of excellent scientists”. Project number: TÁMOP-4.2.2/B-10/1-2010-0012. English was corrected by ProofReading-Service.com. LA - English DB - MTMT ER - TY - JOUR AU - Wang, H -J AU - Zhang, S -C AU - Wang, X -M TI - How to achieve the precise dating of hydrocarbon accumulation JF - NATURAL GAS GEOSCIENCE J2 - NATURAL GAS GEOSCIENCE VL - 24 PY - 2013 IS - 2 SP - 210 EP - 217 PG - 8 SN - 1672-1926 UR - https://m2.mtmt.hu/api/publication/23341571 ID - 23341571 N1 - State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China Research Institute of Petroleum Exploration and Development, Beijing 100083, China Cited By :3 Export Date: 12 February 2021 Correspondence Address: Wang, H.-J.; State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China; email: wanghuajian@petrochina.com.cn State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China Research Institute of Petroleum Exploration and Development, Beijing 100083, China Cited By :3 Export Date: 12 September 2021 Correspondence Address: Wang, H.-J.; State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China; email: wanghuajian@petrochina.com.cn LA - English DB - MTMT ER - TY - JOUR AU - Dolnicek, Z AU - Kropac, K AU - Janickova, K AU - Urubek, T TI - Diagenetic source of fluids causing the hydrothermal alteration of teschenites in the Silesian Unit, Outer Western Carpathians, Czech Republic: Petroleum-bearing vein mineralization from the Stribrnik site JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 37 PY - 2012 IS - 1 SP - 27 EP - 40 PG - 14 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2012.06.004 UR - https://m2.mtmt.hu/api/publication/22671483 ID - 22671483 N1 - Funding Agency and Grant Number: [GACR 205/07/P130] Funding text: P. Gadas (MU Brno) is thanked for assistance during the microprobe work. The stable isotope and organic geochemical analyses conducted by I. jackova, Z. Lnenickova, F. Buzek (CGS Praha), E. Francu, and J. Francu (CGS Brno) are highly appreciated. The detailed comments by two anonymous journal reviewers and associate editor P. Corcoran helped to improve the initial version of the manuscript. The study was supported by project GACR 205/07/P130. Cited By :14 Export Date: 12 February 2021 Correspondence Address: Dolníček, Z.; Department of Geology, 17. listopadu 12, 771 46 Olomouc, Czech Republic; email: dolnicek@prfnw.upol.cz Funding text 1: P. Gadas (MU Brno) is thanked for assistance during the microprobe work. The stable isotope and organic geochemical analyses conducted by I. Jačková, Z. Lněničková, F. Buzek (ČGS Praha), E. Franců, and J. Franců (ČGS Brno) are highly appreciated. The detailed comments by two anonymous journal reviewers and associate editor P. Corcoran helped to improve the initial version of the manuscript. The study was supported by project GAČR 205/07/P130. Cited By :15 Export Date: 12 September 2021 Correspondence Address: Dolníček, Z.; Department of Geology, 17. listopadu 12, 771 46 Olomouc, Czech Republic; email: dolnicek@prfnw.upol.cz LA - English DB - MTMT ER - TY - CHAP AU - George, S.C. AU - Volk, H. AU - Dutkiewicz, A. TI - Mass Spectrometry Techniques for Analysis of Oil and Gas Trapped in Fluid Inclusions T2 - Mass Spectrometry Handbook PB - John Wiley & Sons CY - [s.l.] SN - 9780470536735 PY - 2012 SP - 645 EP - 673 PG - 29 DO - 10.1002/9781118180730.ch30 UR - https://m2.mtmt.hu/api/publication/31867558 ID - 31867558 N1 - Cited By :8 Export Date: 12 February 2021 Correspondence Address: George, S.C.; Department of Earth and Planetary Sciences, , Sydney, NSW, Australia Cited By :8 Export Date: 12 September 2021 Correspondence Address: George, S.C.; Department of Earth and Planetary Sciences, , Sydney, NSW, Australia LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar TI - Geochemistry of Variscan amphibolites from the metamorphic basement of the Körös Complex (Tisza block, Hungary) JF - CARPATHIAN JOURNAL OF EARTH AND ENVIRONMENTAL SCIENCES J2 - CARPATH J EARTH ENVIRON SCI VL - 7 PY - 2012 IS - 3 SP - 5 EP - 18 PG - 14 SN - 1842-4090 UR - https://m2.mtmt.hu/api/publication/1843349 ID - 1843349 N1 - Funding Agency and Grant Number: Szechenyi Foundation; Soros Foundation; OTKA FoundationOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [K60768] Funding text: The XRF analyses were done at Johannes Gutenberg Universitat, Mainz. Special thanks to the Szechenyi and Soros Foundations for supporting the author's research in Mainz, and to R. Oberhansli for making the measurements possible. The REE analyses were made at the Technical University, Budapest by Zs. Molnar. The project was sponsored by the OTKA Foundation (Grant No.: K60768). English was cleaned by the American Journal Experts. Cited By :1 Export Date: 12 February 2021 Correspondence Address: Tóth, T.M.; University of Szeged, Hungary; email: mtoth@geo.u-szeged.hu Cited By :1 Export Date: 12 September 2021 Correspondence Address: Tóth, T.M.; University of Szeged, Hungary; email: mtoth@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Dabi, Gergely AU - Siklósy, Zoltán AU - Schubert, Félix AU - Bajnóczi, Bernadett AU - M. Tóth, Tivadar TI - The relevance of vein texture in understanding the past hydraulic behaviour of a crystalline rock mass: reconstruction of the palaeohydrology of the Mecsekalja Zone, south Hungary JF - GEOFLUIDS J2 - GEOFLUIDS VL - 11 PY - 2011 IS - 3 SP - 309 EP - 327 PG - 19 SN - 1468-8115 DO - 10.1111/j.1468-8123.2011.00342.x UR - https://m2.mtmt.hu/api/publication/1687934 ID - 1687934 LA - English DB - MTMT ER - TY - JOUR AU - Frezzotti, ML Tecce F Casagli A TI - Raman spectroscopy for fluid inclusion analysis JF - JOURNAL OF GEOCHEMICAL EXPLORATION J2 - J GEOCHEM EXPLOR VL - 112 PY - 2011 SP - 1 EP - 20 PG - 20 SN - 0375-6742 DO - 10.1016/j.gexplo.2011.09.009 UR - https://m2.mtmt.hu/api/publication/22027496 ID - 22027496 N1 - Funding Agency and Grant Number: PRINMinistry of Education, Universities and Research (MIUR)Research Projects of National Relevance (PRIN) [2008-BYTF98] Funding text: Present research was in part supported by the PRIN 2008-BYTF98. We acknowledge helpful reviews by R. Thomas and an anonymous reviewer of an earlier version of the manuscript. We are grateful to the Museo di Mineralogia of the University of Rome "La Sapienza" and to the Museo di Mineralogia of the University of Siena for providing several mineral samples for Raman analysis. Raman facilities in Siena were provided by PNRA, the Italian research program for Antarctica. Dipartimento Scienze della Terra, Università di Siena, Via Laterina 8, 53100 Siena, Italy Istituto Geologia Ambientale e Geoingegneria - CNR, C/o Dipartimento Scienze della Terra, Università La Sapienza, P.le Aldo Moro 5, 00185 Roma, Italy Cited By :309 Export Date: 12 February 2021 Correspondence Address: Frezzotti, M.L.; Dipartimento Scienze della Terra, Via Laterina 8, 53100 Siena, Italy; email: marialuce.frezzotti@unisi.it Funding text 1: Present research was in part supported by the PRIN 2008-BYTF98 . We acknowledge helpful reviews by R. Thomas and an anonymous reviewer of an earlier version of the manuscript. We are grateful to the Museo di Mineralogia of the University of Rome “La Sapienza” and to the Museo di Mineralogia of the University of Siena for providing several mineral samples for Raman analysis. Raman facilities in Siena were provided by PNRA, the Italian research program for Antarctica. Dipartimento Scienze della Terra, Università di Siena, Via Laterina 8, 53100 Siena, Italy Istituto Geologia Ambientale e Geoingegneria - CNR, C/o Dipartimento Scienze della Terra, Università La Sapienza, P.le Aldo Moro 5, 00185 Roma, Italy Cited By :351 Export Date: 12 September 2021 Correspondence Address: Frezzotti, M.L.; Dipartimento Scienze della Terra, Via Laterina 8, 53100 Siena, Italy; email: marialuce.frezzotti@unisi.it LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Vass, I TI - Relationship between the geometric parameters of rock fractures, the size of percolation clusters and REV JF - MATHEMATICAL GEOSCIENCES J2 - MATH GEOSCI VL - 43 PY - 2011 IS - 1 SP - 75 EP - 97 PG - 23 SN - 1874-8961 DO - 10.1007/s11004-010-9315-4 UR - https://m2.mtmt.hu/api/publication/1382751 ID - 1382751 LA - English DB - MTMT ER - TY - JOUR AU - Conliffe, J AU - Blamey, N F AU - Feely, M AU - Parnell, J AU - Ryder, A J TI - Hydrocarbon migration in the Porcupine Basin, offshore Ireland: evidence from fluid inclusion studies. JF - PETROLEUM GEOSCIENCE J2 - PETROL GEOSCI VL - 16 PY - 2010 IS - 1 SP - 67 EP - 76 PG - 10 SN - 1354-0793 DO - 10.1144/1354-079309-007 UR - https://m2.mtmt.hu/api/publication/20982832 ID - 20982832 N1 - Funding Agency and Grant Number: Science Foundation of Ireland Research Frontiers ProgramScience Foundation Ireland [05/RFP/GEO0002] Funding text: The fluorescence lifetime analysis was funded under a Science Foundation of Ireland Research Frontiers Program, Grant no: (05/RFP/GEO0002) to AGR. Cited By :19 Export Date: 12 February 2021 Correspondence Address: Conliffe, J.; Department of Earth Sciences, , St John's, NL A1B 3X5, Canada; email: jamesconliffe@mun.ca Cited By :22 Export Date: 12 September 2021 Correspondence Address: Conliffe, J.; Department of Earth Sciences, , St John's, NL A1B 3X5, Canada; email: jamesconliffe@mun.ca LA - English DB - MTMT ER - TY - THES AU - Hanson, Stacey Leigh TI - Structure and vein isotopic signatures of a cambro-ordovician 360M core from Saratoga Springs region, New York state: Implications for tectonics, gas exploration, and CO2 sequestration PY - 2010 SN - 9781124244457 UR - https://m2.mtmt.hu/api/publication/34621509 ID - 34621509 LA - English DB - MTMT ER - TY - JOUR AU - Suchý, V AU - Dobeš, P AU - Sýkorová, I AU - Machovič, V AU - Stejskal, M AU - Kroufek, J AU - Chudoba, J AU - Matějovský, L AU - Havelcová, M AU - Matysová, P TI - Oil-bearing inclusions in vein quartz and calcite and, bitumens in veins: Testament to multiple phases of hydrocarbon migration in the Barrandian basin (lower Palaeozoic), Czech Republic. JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 27 PY - 2010 IS - 1 SP - 285 EP - 297 PG - 13 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2009.08.017 UR - https://m2.mtmt.hu/api/publication/20982836 ID - 20982836 N1 - Funding Agency and Grant Number: Academy of Sciences of the Czech RepublicCzech Academy of Sciences [A3012703/1997, IAA 300460804]; IRSM [304605519] Funding text: We dedicate this paper to the memory of Doc. Ing. Michal Stejskal, CSc. (1947-2007), our respected colleague and friend, who pioneered the use of modern organic-geochemical techniques to study the petroleum geology of the Czech Republic. He made a significant intellectual contribution to the present work but did not have the pleasure of seeing the resulting paper published. We further wish to acknowledge the Grant Agency of the Academy of Sciences of the Czech Republic (Research Grants A3012703/1997 and IAA 300460804) and the funding of IRSM (Research Plan A VOZ 304605519) for supporting this study. The authors are grateful to Dr. Martin Feely (NUI Galway, Ireland) for critically reviewing and correcting the manuscript. Jiránkova 1136/4, 163 00 Prague 6, Czech Republic Czech Geological Survey, Klárov 3/131, P.O. Box 85, 118 21 Prague 1, Czech Republic Institute of Rock Structure and Mechanics, Academy of Sciences of the Czech Republic, V Holešovičkách, 182 09 Prague 8, Czech Republic Institute of Chemical Technology, Technická 5, 166 28 Prague 6, Czech Republic Cited By :26 Export Date: 12 February 2021 Correspondence Address: Suchý, V.; Jiránkova 1136/4, 163 00 Prague 6, Czech Republic; email: sediment@quick.cz Funding details: VOZ 304605519 Funding details: Akademie Věd České Republiky, AV ČR, IAA 300460804, A3012703/1997 Funding text 1: We dedicate this paper to the memory of Doc. Ing. Michal Stejskal, CSc. (1947–2007), our respected colleague and friend, who pioneered the use of modern organic-geochemical techniques to study the petroleum geology of the Czech Republic. He made a significant intellectual contribution to the present work but did not have the pleasure of seeing the resulting paper published. We further wish to acknowledge the Grant Agency of the Academy of Sciences of the Czech Republic (Research Grants A3012703/1997 and IAA 300460804) and the funding of IRSM (Research Plan A VOZ 304605519) for supporting this study. The authors are grateful to Dr. Martin Feely (NUI Galway, Ireland) for critically reviewing and correcting the manuscript. Jiránkova 1136/4, 163 00 Prague 6, Czech Republic Czech Geological Survey, Klárov 3/131, P.O. Box 85, 118 21 Prague 1, Czech Republic Institute of Rock Structure and Mechanics, Academy of Sciences of the Czech Republic, V Holešovičkách, 182 09 Prague 8, Czech Republic Institute of Chemical Technology, Technická 5, 166 28 Prague 6, Czech Republic Cited By :27 Export Date: 12 September 2021 Correspondence Address: Suchý, V.; Jiránkova 1136/4, 163 00 Prague 6, Czech Republic; email: sediment@quick.cz Funding details: VOZ 304605519 Funding details: Akademie Věd České Republiky, AV ČR, A3012703/1997, IAA 300460804 Funding text 1: We dedicate this paper to the memory of Doc. Ing. Michal Stejskal, CSc. (1947–2007), our respected colleague and friend, who pioneered the use of modern organic-geochemical techniques to study the petroleum geology of the Czech Republic. He made a significant intellectual contribution to the present work but did not have the pleasure of seeing the resulting paper published. We further wish to acknowledge the Grant Agency of the Academy of Sciences of the Czech Republic (Research Grants A3012703/1997 and IAA 300460804) and the funding of IRSM (Research Plan A VOZ 304605519) for supporting this study. The authors are grateful to Dr. Martin Feely (NUI Galway, Ireland) for critically reviewing and correcting the manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Volk, H AU - Fuentes, D AU - Fuerbach, A AU - Miese, C AU - Koehler, W AU - Bärsch, N AU - Barcikowski, S TI - First on-line analysis of petroleum from single inclusion using ultrafast laser ablation. JF - ORGANIC GEOCHEMISTRY J2 - ORG GEOCHEM VL - 41 PY - 2010 IS - 2 SP - 74 EP - 77 PG - 4 SN - 0146-6380 DO - 10.1016/j.orggeochem.2009.05.006 UR - https://m2.mtmt.hu/api/publication/20982838 ID - 20982838 N1 - CSIRO Petroleum, North Ryde, Sydney, NSW 2113, Australia MQPhotonics Research Centre, Macquarie University, Sydney, NSW 2119, Australia Femtolasers Produktions GmbH, Fernkornagasse 10, 1100 Wien, Austria Laser Zentrum Hannover e.V., Hollerithallee 8, 30419 Hannover, Germany Cited By :27 Export Date: 12 February 2021 CODEN: ORGED Correspondence Address: Volk, H.; CSIRO Petroleum, North Ryde, Sydney, NSW 2113, Australia; email: Herbert.Volk@csiro.au CSIRO Petroleum, North Ryde, Sydney, NSW 2113, Australia MQPhotonics Research Centre, Macquarie University, Sydney, NSW 2119, Australia Femtolasers Produktions GmbH, Fernkornagasse 10, 1100 Wien, Austria Laser Zentrum Hannover e.V., Hollerithallee 8, 30419 Hannover, Germany Cited By :29 Export Date: 12 September 2021 CODEN: ORGED Correspondence Address: Volk, H.; CSIRO Petroleum, North Ryde, Sydney, NSW 2113, Australia; email: Herbert.Volk@csiro.au LA - English DB - MTMT ER - TY - JOUR AU - Ryder, A G AU - Blamey, N J F TI - Hydrocarbon Fluid Inclusion Fluorescence: A review. VL - 4 PY - 2009 SP - 299 EP - 334 PG - 36 UR - https://m2.mtmt.hu/api/publication/20982833 ID - 20982833 LA - English DB - MTMT ER - TY - JOUR AU - Szabó, B AU - Schubert, Félix AU - M. Tóth, Tivadar TI - Paleofluid evolution of the fractured basalt hydrocarbon reservoir in the Üllés–Ruzsa–Bordány area, SE Hungary JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 52 PY - 2009 IS - 3-4 SP - 299 EP - 323 PG - 25 SN - 1788-2281 DO - 10.1556/CEuGeol.52.2009.3-4.6 UR - https://m2.mtmt.hu/api/publication/1382753 ID - 1382753 LA - English DB - MTMT ER - TY - CHAP AU - Szabó, B AU - Hetényi, Magdolna AU - Schubert, Félix AU - Milota, K AU - M. Tóth, Tivadar ED - M. Tóth, Tivadar TI - Repedezett bazalt anyagú szénhidrogén rezervoárok Üllés-Bordány térségében. T2 - Magmás és metamorf képződmények a Tiszai Egységben PB - SZTE TTIK Földrajzi és Földtani Tanszékcsoport CY - Szeged SN - 9789634829782 T3 - GeoLitera, ISSN 2060-7067 PY - 2009 SP - 307 EP - 323 PG - 17 UR - https://m2.mtmt.hu/api/publication/1287366 ID - 1287366 LA - Hungarian DB - MTMT ER - TY - CHAP AU - Vass, I AU - M. Tóth, Tivadar AU - Szanyi, János AU - Kovács, Balázs ED - M. Tóth, Tivadar TI - Az aljzati kristályos hátak szerepe az Alföld fluidum áramlási és hőtranszport folyamataiban T2 - Magmás és metamorf képződmények a Tiszai Egységben PB - SZTE TTIK Földrajzi és Földtani Tanszékcsoport CY - Szeged SN - 9789634829782 T3 - GeoLitera, ISSN 2060-7067 PY - 2009 SP - 325 EP - 339 PG - 15 UR - https://m2.mtmt.hu/api/publication/1382869 ID - 1382869 LA - Hungarian DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Redlerné, Tátrai M AU - Kummer, I TI - A Szeghalom környéki metamorf aljzat kiemelkedés szerkezetfejlődése és felépítése kőzettani és szeizmikus adatok alapján [Structural evolution of the Szeghalom metamorphic dome on the basis of petrological and seismic data] JF - MAGYAR GEOFIZIKA J2 - MAGYAR GEOFIZIKA VL - 49 PY - 2008 IS - 4 SP - 143 EP - 151 PG - 9 SN - 0025-0120 UR - https://m2.mtmt.hu/api/publication/1348922 ID - 1348922 N1 - Szegedi Tudományegyetem Ásványtani, Geokémiai és Kozettani Tanszék, H-6722 Szeged, Egyetem u. 2 Magyar Állami Eötvös Loránd Geofizikai Intézet, H-1145 Budapest, Kolumbusz u. 17-23 Cited By :2 Export Date: 12 February 2021 Correspondence Address: Tivadar, M. T.; Szegedi Tudományegyetem Ásványtani, , H-6722 Szeged, Egyetem u. 2; email: mtoth@geo.u-szeged.hu Szegedi Tudományegyetem Ásványtani, Geokémiai és Kozettani Tanszék, H-6722 Szeged, Egyetem u. 2 Magyar Állami Eötvös Loránd Geofizikai Intézet, H-1145 Budapest, Kolumbusz u. 17-23 Cited By :3 Export Date: 12 September 2021 Correspondence Address: Tivadar, M. T.; Szegedi Tudományegyetem Ásványtani, , H-6722 Szeged, Egyetem u. 2; email: mtoth@geo.u-szeged.hu LA - Hungarian DB - MTMT ER - TY - JOUR AU - Kovács, Balázs AU - Szanyi, János AU - M. Tóth, Tivadar AU - Vass, I TI - Geothermal heat potential of Hungary with special regards to high enthalpy basement JF - PUBLICATIONS OF THE UNIVERSITY OF MISKOLC SERIES A-MINING J2 - PUBL UNIV MISKOLC SER A MIN VL - 72 PY - 2007 SP - 81 EP - 94 PG - 14 SN - 1219-008X UR - https://m2.mtmt.hu/api/publication/1129830 ID - 1129830 LA - English DB - MTMT ER - TY - CHAP AU - M. Tóth, Tivadar AU - Vass, I AU - Szanyi, János AU - Kovács, Balázs ED - Ribeiro, L ED - Chambel, A ED - Condesso, de Melo M T TI - Water and heat flow through uplifted metamorphic highs in the basement of the Pannonian Basin T2 - XXXV. Congress of International Association of Hydrogeologists PB - International Association of Hydrogeologists (IAH) CY - Lisszabon SN - 9789899529731 PY - 2007 SP - 503 EP - 512 PG - 10 UR - https://m2.mtmt.hu/api/publication/1129829 ID - 1129829 LA - English DB - MTMT ER -