TY - CHAP AU - Nandakumar, V. AU - Jayanthi, J.L. TI - Nondestructive analytical techniques for fluid inclusions T2 - Hydrocarbon Fluid Inclusions in Petroliferous Basins PB - Elsevier CY - Amsterdam SN - 9780128174173 PY - 2021 SP - 31 EP - 74 PG - 44 DO - 10.1016/B978-0-12-817416-6.00004-6 UR - https://m2.mtmt.hu/api/publication/32343998 ID - 32343998 LA - English DB - MTMT ER - TY - JOUR AU - Bai, X. AU - Hao, G. AU - Shan, X. AU - Zeng, Z. AU - Liu, Y. TI - Developmental Pattern of Metamorphic Rock Burial Hill Reservoirs in Central Uplift of Songliao Basin JF - Xi'an Shiyou Daxue Xuebao (Ziran Kexue Ban)/Journal of Xi'an Shiyou University, Natural Sciences Edition J2 - Journal of Xian Shiyou University VL - 35 PY - 2020 IS - 3 SP - 28 EP - 38 PG - 11 SN - 1673-064X DO - 10.3969/j.issn.1673-064X.2020.03.004 UR - https://m2.mtmt.hu/api/publication/31867584 ID - 31867584 N1 - School of Geosciences, Jilin University, Changchun, Jilin 130012, China China Center for Aerial Geophysical Exploration and Remote Sensing of Natural Resources, Beijing, 100083, China Export Date: 12 February 2021 Correspondence Address: Hao, G.; School of Geosciences, China; email: haoguoli@jlu.edu.cn AB - The characteristics, development patters and forming mechanism of the middle-shallow metamorphic buried hill reservoir in the central uplift belt of Songliao Basin are studied based on drilling core, casting thin section, zircon dating, logging and gas testing data. It is shown that the metamorphic buried hill reservoir is mainly distributed in the metamorphic glutenite, schist, cataclastic granite, mylonite. The reservoir is mainly divided into two types: weathered crust and inner layer. The weathered crust reservoir is developed at the top of the uplift zone, mainly developed dissolution fractures and broken intergranular pores; the lower part of the weathered crust is an insider type reservoir, which can be divided into two sets (insider I and insider II) under the influence of different longitudinal lithology. In insider I, structural fractures (1.1%~3.2%), intergranular pores (0.3%~1.4%) and intragranular corrosion pores (0.1%~0.8%) are mainly developed; in insider II, foliation fractures (0.5%~1.2%) and local intragranular dissolution pores (0.3%~0.7%) are mainly developed. The physical property and gas bearing property of weathered crust type reservoir are better than that of inside type reservoir. The main forming mechanism of metamorphic buried hill reservoir in the study area is dissolution and uplift extrusion. The main reason for the undevelopment of reservoir in deep insider I is that the reservoir pores are reduced or even completely filled due to the burial depth and hydrothermal process. © 2020, the Editorial Department of Journal of Xi'an Shiyou University. All right reserved. LA - Chinese DB - MTMT ER - TY - JOUR AU - Fodor, László TI - Results, problems and future tasks of palaeostress and fault-slip analyses in the Pannonian Basin: the Hungarian contribution JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 149 PY - 2019 IS - 4 SP - 297 EP - 326 PG - 30 SN - 0015-542X DO - 10.23928/foldt.kozl.2019.149.4.297 UR - https://m2.mtmt.hu/api/publication/30852034 ID - 30852034 N1 - Export Date: 27 November 2019 Correspondence Address: Fodor, L.; MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/C, Hungary; email: lasz.Fodor@yahoo.com LA - English DB - MTMT ER - TY - CHAP AU - Noah, M. AU - Volk, H. AU - Schubert, F. AU - Horsfield, B. TI - Identification of NSO compounds trapped in fluid inclusions using FT-ICR-MS -a case study from the Pannonian Basin (Hungary) PB - European Association of Geoscientists and Engineers (EAGE) SN - 9789462823044 PY - 2019 SP - 1 EP - 2 PG - 2 DO - 10.3997/2214-4609.201903036 UR - https://m2.mtmt.hu/api/publication/31867585 ID - 31867585 N1 - Shell Conference code: 152636 Export Date: 12 February 2021 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 - Wang, C. AU - Liu, H. AU - Feng, H. AU - Deng, J. AU - Liu, X. AU - Zhao, F. TI - Geochemistry and U-Pb ages of the diabases from the Luoji area, western Yunnan, China: Implications for the timing of the initial rifting of the Ganzi-Litang Ocean JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 72 PY - 2019 IS - Special Issue SP - 19 EP - 32 PG - 14 SN - 1330-030X DO - 10.4154/gc.2019.25 UR - https://m2.mtmt.hu/api/publication/31146241 ID - 31146241 N1 - Chengdu University of Technology, College of Earth Sciences, Chengdu, Sichuan 610059, China School of Environment and Earth Science, University of Queensland, Brisbane, QLD 4072, Australia Chengdu University of Technology, College of Energy, State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu, Sichuan 610059, China North China Petroleum Administration Co., Ltd, Sulige Exploration and Development Branch, Shijiazhuang, Hebei 017300, China Export Date: 29 January 2020 Correspondence Address: Liu, H.; School of Environment and Earth Science, University of QueenslandAustralia; email: 277515537@qq.com Chengdu University of Technology, College of Earth Sciences, Chengdu, Sichuan 610059, China School of Environment and Earth Science, University of Queensland, Brisbane, QLD 4072, Australia Chengdu University of Technology, College of Energy, State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu, Sichuan 610059, China North China Petroleum Administration Co., Ltd, Sulige Exploration and Development Branch, Shijiazhuang, Hebei 017300, China Export Date: 12 February 2021 Correspondence Address: Liu, H.; School of Environment and Earth Science, Australia; email: 277515537@qq.com AB - Detailed geochemical and U-Pb studies of two diabases (Luoji and Cuiyi) from the Luoji area have been undertaken. The diabases are high-K calc-alkaline and belonging to the tholeiitic series, enriched in large ion lithophile elements, Ti, Zr and light rare earth elements, and depleted in high field strength elements. These characteristics are different from the oceanic island basalt but highly consistent with the continental rift basalt, indicating the Luoji and Cuiyi diabases are the products of the intracontinental rift related to the initial opening of the Ganzi-Litang Ocean. The Luoji and Cuiyi diabases originated from an enriched mantle source with a small degree of crustal contamination during their emplacement. Zircon U-Pb ages show that the Luoji and Cuiyi diabases were emplaced at 293.4±5.4Ma. Therefore, we propose that the time of initial rifting of the Ganzi-Litang Ocean occurred during the very Early Permian. © 2019, Croatian Geological Survey. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Abd Rahman, Norhan AU - Foong, Loke Kok AU - Nazir, Ramli AU - Lewis, Roland W. TI - Vibration effect influence upon non-aqueous phase liquid migration in double-porosity soil JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 71 PY - 2018 IS - 3 SP - 163 EP - 171 PG - 9 SN - 1330-030X DO - 10.4154/gc.2018.14 UR - https://m2.mtmt.hu/api/publication/30598514 ID - 30598514 N1 - Universiti Teknologi Malaysia, Faculty of Civil Engineering, Centre of Tropical GeoengineeringJohor, Malaysia Universiti Teknologi Malaysia, Faculty of Civil EngineeringJohor, Malaysia University of Wales Swansea, School of Engineering, Swansea, W. Glam, SA2 8PP, United Kingdom Cited By :1 Export Date: 12 February 2021 Correspondence Address: Rahman, N.A.; Universiti Teknologi Malaysia, Malaysia; email: norhan@utm.my Funding details: Ministry of Higher Education, Malaysia, MOHE Funding details: Universiti Teknologi Malaysia, UTM, PY/2016/06547 Funding text 1: This study was supported by the Research Management Centre (RMC), Universiti Teknologi Malaysia under Research University Grant – Tier 1 (PY/2016/06547) from the Ministry of Higher Education Malaysia. The authors would also like to thank their respective University, Public Service Department Malaysia, Geotechnical Laboratory, Hydraulic and Hydrology Laboratory, Engineering Seismology and Earthquake Engineering Research Group (eSEER), and Survey Unit, Faculty of Civil Engineering, Universiti Teknologi Malaysia for kind assistance lent to this research. The second author was supported through the federal training award by the Public Service Department under Prime Minister’s Department, Malaysia. AB - Natural disasters such as earthquakes, El-Nino, tsunamis and water pollution have a negative impact on human health and living environment. Some of these may give rise to subsurface vibrations that can potentially increase groundwater pollution risks in double-porosity systems. The more complicated situation was where underground storage tanks and petroleum pipeline damage have caused the leakage of non-aqueous phase liquids (NAPLs) which migrated into the groundwater resources. These problems need to be addressed by both professionals and researchers worldwide to ensure the sustainability of groundwater utilization. This paper aims to investigate and understand NAPL migration in vibrated double-porosity soils. To do so it was necessary to study the phenomena and characteristic of soil structure and the pattern of NAPL migration to identify cost-effective remediation schemes. A laboratory experiment was conducted to study the phenomena and characteristics of vibration response and NAPL migration in double-porosity soil deformation under vibration effect using a digital image processing technique (DIPT). The outcomes of the experiment show that the gradual increase of vibration table excitation frequency yielded different vibration responses from the respective soils. This indicated that soil surface acceleration depended significantly on the soil conditions, soil water content, soil structure and the pattern of soil fracturing. NAPL migration was faster in sample 2 with 150ml toluene than sample 1 with 70ml toluene and this could be because the greater amount of toluene in sample 2 exerted an extra entry force on top of the soil sample that had yet to migrate through the sample surface. Finally, it was concluded that the DIPT may provide detailed information, and can be used to understand and identify the remediation method as well as to ensure the sustainable consumption of groundwater. 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 -