TY - BOOK ED - Babinszki, Edit ED - Piros, Olga ED - Budai, Tamás ED - Gyalog, László ED - Halász, Amadé ED - Király, Edit ED - Koroknai, B ED - Haranginé Lukács, Réka ED - M. Tóth, Tivadar TI - Magyarország litosztratigráfiai egységeinek leírása I.. Prekainozoos képződmények TS - Prekainozoos képződmények PB - Szabályozott Tevékenységek Felügyeleti Hatósága CY - Budapest PY - 2023 SP - 275 SN - 9789636713263 UR - https://m2.mtmt.hu/api/publication/33825476 ID - 33825476 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Raucsikné Varga, Andrea Beáta AU - Pál-Molnár, Elemér AU - Raucsik, Béla TI - Revealing the Mineralogical and Petrographic Signs of Fluid-Related Processes in the Kelebia Basement Area (Szeged Basin, S Hungary): A Case Study of Alpine Prograde Metamorphism in a Permo-Triassic Succession JF - GEOFLUIDS J2 - GEOFLUIDS VL - 2023 PY - 2023 SP - 1 EP - 18 PG - 18 SN - 1468-8115 DO - 10.1155/2023/8600576 UR - https://m2.mtmt.hu/api/publication/33594461 ID - 33594461 N1 - This work was financially supported by the University of Szeged Open Access Fund (4635), the Bolyai Research Scholarship of the Hungarian Academy of Sciences (BO/266/18), and the National Research, Development, and Innovation Fund (projects no. K 108375 and K 131690). AB - The Szeged Basin (S Hungary) occupies a relatively central position within the European Alpine–Carpathian–Dinaride orogenic belt. An ongoing controversy about the tectonic position of the study area indicates that its evolution is still not fully understood; however, several important hydrocarbon occurrences are known in the fractured basement reservoirs. The main aim of this contribution is to investigate the petrographic features and possible Alpine metamorphic conditions of volcanic/volcanoclastic and siliciclastic rocks from the Kelebia basement area. Due to the outcrop conditions and poor exposure, study samples are obtained from cores and core chips resulting from oil exploration. Based on an evaluation of petrographic (including also cathodoluminescence analysis) and microstructural features, joined with mineralogical and metamorphic data such as “illite crystallinity” and K-white mica crystallite size obtained by X-ray powder diffractometry (XRPD), a very low- to low-grade (ca. 300°C) Alpine metamorphic imprint of this portion of the basement can be proposed. Several deformation characteristics (deformation lamellae in quartz, deformation twins in dolomite, fragmented porphyroclasts, and strain shadows) were recognized in the studied samples, showing a weakly to moderately developed disjunctive foliation in the Permian rocks, as well as quartz veinlets, microcracks, and fluid inclusion planes in the Lower Triassic sandstones. Most likely, one of the Cretaceous orogenic events, namely, the “Turonian” phase (Early–Late Cretaceous nappe stacking), resulted in the prograde greenschist facies metamorphism in the study area, instead of the burial depth. We propose that the Permo-Triassic cover succession was also affected by shearing episodes accompanied by fluid migrations along the contact zone between the tectonic units. The scientific approach and dataset provided here are examples of how the application of XRPD parameters of phyllosilicates and micropetrographic observations can help to understand the evolution of an orogen and improve knowledge about the basement structure. LA - English DB - MTMT ER - TY - JOUR AU - Wang, S AU - Ma, C AU - Sun, X AU - Liu, S TI - Lacustrine Shale Diagenesis—A Case Study of the Second Member of the Funing Formation in the Subei Basin JF - PROCESSES J2 - PROCESSES VL - 11 PY - 2023 IS - 7 SN - 2227-9717 DO - 10.3390/pr11072009 UR - https://m2.mtmt.hu/api/publication/34053465 ID - 34053465 AB - Shale diagenesis differs from that of sandstone and carbonate rocks with regard to the type, evolution stage, and evolution mode. The quality of shale reservoirs is closely linked to the extent of diagenetic evolution. This study identifies the types and characteristics of shale diagenesis using thin sections and scanning electron microscopy (SEM) observations. The stages of shale diagenesis are determined by analyzing organic matter evolution and clay mineral transformation and establishing a diagenetic evolution sequence. This paper describes the comprehensive diagenetic evolution of organic matter, clay minerals, clastic particles, and carbonate minerals to determine the diagenesis types, diagenetic sequences, and pore evolution occurring during diagenetic evolution. The results show that the diagenesis types of shale in the second member of the Funing Formation include compaction, dissolution, cementation, metasomatism, dolomitization, syneresis, and transformation of clay minerals, as well as thermal evolution of organic matter. The middle diagenetic A stage is prevalent, with some areas in the early and middle diagenetic B stages. The shale underwent a diagenetic evolution sequence, including the collapse and shrinkage of montmorillonite interlayers in the early stage; the rapid formation and transformation of illite and smectite mixed layers, massive hydrocarbon generation of organic matters, and dissolution of unstable components in the middle stage; and the occurrence of fractures filled with gypsum, quartz, ferrocalcite, or other authigenic minerals in the later stage. Dissolution pores and fractures are the dominant shale reservoirs of the second member of the Funing Formation in the Subei Basin. The results provide new insights into understanding the formation and evolution of reservoir spaces during shale diagenesis and information for the exploration and development of lacustrine shale oil and gas. LA - English DB - MTMT ER - TY - JOUR AU - Wang, W AU - Li, C AU - Dodd, MS. AU - Algeo, TJ. AU - Zhang, Z AU - Cheng, M AU - Hou, M TI - A DOM regulation model for dolomite versus calcite precipitation in the Ediacaran ocean: Implications for the “dolomite problem” JF - PRECAMBRIAN RESEARCH J2 - PRECAMBRIAN RES VL - 385 PY - 2023 SN - 0301-9268 DO - 10.1016/j.precamres.2022.106947 UR - https://m2.mtmt.hu/api/publication/33538610 ID - 33538610 LA - English DB - MTMT ER - TY - JOUR AU - Zhu, G AU - Li, X AU - Li, T AU - Zhou, L AU - Wu, Y AU - Shen, B AU - Ning, M TI - Magnesium isotope trace dolomitization fluid migration path: A case study of the Carboniferous Huanglong Formation in the Sichuan basin JF - ACTA GEOLOGICA SINICA J2 - ACTA GEOLOGICA SINICA VL - 97 PY - 2023 IS - 3 SP - 753 EP - 771 PG - 19 SN - 0001-5717 DO - 10.19762/j.cnki.dizhixuebao.2022057 UR - https://m2.mtmt.hu/api/publication/34011869 ID - 34011869 LA - Multilingual DB - MTMT ER - TY - JOUR AU - Zhu, G AU - Li, X TI - Progress in genetic types and research methods of dolomite JF - Shiyou Xuebao/Acta Petrolei Sinica J2 - Shiyou Xuebao/Acta Petrolei Sinica VL - 44 PY - 2023 IS - 7 SP - 1167 EP - 1190 PG - 24 SN - 0253-2697 DO - 10.7623/syxb202307012 UR - https://m2.mtmt.hu/api/publication/34181718 ID - 34181718 LA - Chinese DB - MTMT ER - TY - JOUR AU - Centrella, S AU - Beaudoin, NE. AU - Koehn, D AU - Motte, G AU - Hoareau, G AU - Callot, JP TI - How fluid-mediated rock transformations can mimic hydro-fracturing patterns in hydrothermal dolomite JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 140 PY - 2022 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2022.105657 UR - https://m2.mtmt.hu/api/publication/32771241 ID - 32771241 LA - English DB - MTMT ER - TY - JOUR AU - Li, K AU - Cai, C AU - Tan, X AU - Jiang, H AU - Fan, J TI - Multiple fluid flow events and diversity of hydrothermal minerals in Neoproterozoic to lower Paleozoic carbonate reservoirs, Tarim Basin, NW China JF - JOURNAL OF ASIAN EARTH SCIENCES J2 - J ASIAN EARTH SCI VL - 233 PY - 2022 SN - 1367-9120 DO - 10.1016/j.jseaes.2022.105260 UR - https://m2.mtmt.hu/api/publication/32823659 ID - 32823659 LA - English DB - MTMT ER - TY - JOUR AU - Li, X AU - Lehrmann, DJ. AU - Luczaj, J AU - Kelley, BM. AU - Cantrell, DL. AU - Yu, M AU - Ferrill, NL AU - Payne, JL. TI - Unraveling overprinted formation mechanisms of massive dolostone in the Lower Triassic sequence of an isolated carbonate platform in Nanpanjiang Basin, south China JF - SEDIMENTARY GEOLOGY J2 - SEDIMENT GEOL VL - 440 PY - 2022 SN - 0037-0738 DO - 10.1016/j.sedgeo.2022.106240 UR - https://m2.mtmt.hu/api/publication/33098794 ID - 33098794 N1 - Department of Geological Sciences, Stanford University, Stanford, CA 94305, United States Department of Geosciences, Trinity University, San Antonio, TX 78212, United States Department of Natural & Applied Sciences, University of Wisconsin-Green Bay, Green Bay, WI 54311, United States Department of Geosciences, The Pennsylvania State University, University ParkPA 16802, United States Cantrell GeoLogic, Franklin, TN 37069, United States Department of Resources & Environmental Engineering, Guizhou University, Guizhou Province, Guiyang, 550025, China Export Date: 24 January 2023 Correspondence Address: Li, X.; Department of Geological Sciences, United States; email: geo.xwli@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Noorian, Y AU - Moussavi-Harami, R AU - Hollis, C AU - Reijmer, JJG. AU - Mahboubi, A AU - Omidpour, A TI - Control of climate, sea-level fluctuations and tectonics on the pervasive dolomitization and porosity evolution of the Oligo-Miocene Asmari Formation (Dezful Embayment, SW Iran) JF - SEDIMENTARY GEOLOGY J2 - SEDIMENT GEOL VL - 427 PY - 2022 SN - 0037-0738 DO - 10.1016/j.sedgeo.2021.106048 UR - https://m2.mtmt.hu/api/publication/32533869 ID - 32533869 LA - English DB - MTMT ER - TY - JOUR AU - Ryan, BH AU - Kaczmarek, SE AU - Rivers, JM AU - Manche, CJ TI - Extensive recrystallization of Cenozoic dolomite during shallow burial: A case study from the Palaeocene–Eocene Umm er Radhuma formation and a global meta-analysis JF - SEDIMENTOLOGY J2 - SEDIMENTOLOGY VL - 69 PY - 2022 IS - 5 SP - 2053 EP - 2079 PG - 27 SN - 0037-0746 DO - 10.1111/sed.12982 UR - https://m2.mtmt.hu/api/publication/32737944 ID - 32737944 AB - Recrystallization of dolomite can alter textural, mineralogical and geochemical attributes used to infer environmental conditions of initial dolomitization. A meta-analysis of the published literature shows that extensive recrystallization is most common in old and deeply buried dolomites, but data from the Palaeocene–Eocene Umm er Radhuma Formation in Qatar show that this can also happen in geologically young carbonates that have never been deeply buried. Evidence of extensive recrystallization comes from a principal component analysis of published mineralogical and geochemical data that are integrated with new clumped isotope (∆47) measurements and cathodoluminescence petrography. The observations indicate that dolomite stoichiometry and cation ordering correlate with dolomite texture and depth: shallow mimetic dolomites are less stoichiometric and poorly-ordered whereas coarser and deeper planar-e and planar-s to nonplanar dolomites with mottled cathodoluminescence signatures are more stoichiometric and well-ordered, suggesting they have recrystallized. Dolomite δ18O data (Vienna Pee Dee Belemnite) also covary with texture, as mimetic dolomites have the narrowest range (−0.45‰ to +0.38‰), planar-e dolomites are generally ≤0‰ (−2.4‰ to +0.68‰) and planar-s to nonplanar dolomites exhibit the widest range (−2.3‰ to +1.4‰). The principal component analysis results indicate one component with positive loadings for dolomite stoichiometry (+0.752) and cation ordering (+0.813), and negative loading for δ18O (−0.833), trends predicted in recrystallized dolomites. The ∆47-derived temperatures (32 to 46°C) and δ18Ow (+0.18 to +2.6‰ Vienna Standard Mean Ocean Water) reflect recrystallization by warm, slightly evaporated seawater at shallow depths. In the context of a meta-analysis of recrystallized dolomites in the literature, this study implies that extensive dolomite recrystallization in Cenozoic dolomites and shallow-burial conditions is an under-appreciated phenomenon. The results of this study also demonstrate that initial petrological attributes can be significantly altered after dolomitization, hindering interpretations of past seawater chemistry and environmental conditions of dolomitization. LA - English DB - MTMT ER - TY - JOUR AU - Ahmad, W AU - Ullah, S AU - Ahmad, I AU - Gingras, MK. AU - Shafique, M AU - Khan, EU AU - Shah, Mumtaz TI - Reflux dolomitization and subsequent hydrothermal dolomitization induced by the Alkaline Igneous Province in the Middle Devonian Nowshera Formation (Peshawar Basin, NW Pakistan) JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 131 PY - 2021 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2021.105178 UR - https://m2.mtmt.hu/api/publication/32106701 ID - 32106701 LA - English DB - MTMT ER - TY - JOUR AU - Barale, L. AU - Bertok, C. AU - D’atri, A. AU - Piana, F. AU - Bernasconi, S.M. AU - Czuppon, György AU - Palcsu, László AU - Gerdes, A. AU - Birgel, D. AU - Martire, L. TI - U-pb dating and geochemical constraints to early cretaceous hydrothermal dolomitization in the provenÇal domain (Maritime alps, nw italy-se france) JF - OFIOLITI J2 - OFIOLITI VL - 46 PY - 2021 IS - 2 SP - 131 EP - 149 PG - 19 SN - 0391-2612 DO - 10.4454/ofioliti.v46i2.543 UR - https://m2.mtmt.hu/api/publication/32089112 ID - 32089112 N1 - National Research Council of Italy, Institute of Geosciences and Earth Resources, Torino, Italy University of Torino, Department of Earth Sciences, Torino, Italy ETH Zurich, Department of Earth Sciences, Zurich, Switzerland Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network, Budapest, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Debrecen, Hungary Goethe University Frankfurt, Department of Geosciences, Frankfurt am Main, Germany University of Hamburg, Department of Earth Sciences, Institute for Geology, Hamburg, Germany Export Date: 2 July 2021 Correspondence Address: Bertok, C.; University of Torino, Italy; email: carlo.bertok@unito.it LA - English DB - MTMT ER - TY - JOUR AU - Cai, WK AU - Liu, JH AU - Zhou, CH AU - Keeling, J AU - Glasmacher, UA. TI - Structure, genesis and resources efficiency of dolomite: New insights and remaining enigmas JF - CHEMICAL GEOLOGY J2 - CHEM GEOL VL - 573 PY - 2021 SN - 0009-2541 DO - 10.1016/j.chemgeo.2021.120191 UR - https://m2.mtmt.hu/api/publication/31933741 ID - 31933741 LA - English DB - MTMT ER - TY - JOUR AU - Hou, Z. AU - Zhou, L. AU - Jin, F. AU - Chen, S. AU - Pu, X. AU - Yan, J. AU - Li, H. TI - Hydrothermal Fluid Activity and Its Reformation on Reservoirs in Qikou Depression JF - DIQIU KEXUE / EARTH SCIENCE: JOURNAL OF CHINA UNIVERSITY OF GEOSCIENCES J2 - EARTH SCI J CHINA UNIV GEOSCI VL - 46 PY - 2021 IS - 1 SP - 200 EP - 214 PG - 15 SN - 1000-2383 DO - 10.3799/dqkx.2019.282 UR - https://m2.mtmt.hu/api/publication/31876066 ID - 31876066 LA - English DB - MTMT ER - TY - JOUR AU - Mandal, A AU - Tripathy, GR AU - Goswami, V AU - Ackerman, L AU - Parcha, SK. AU - Chandra, R TI - Re–Os and Sr Isotopic Study of Permian–Triassic Sedimentary Rocks from the Himalaya: Shale Chronology and Carbonate Diagenesis JF - MINERALS J2 - MINERALS-BASEL VL - 11 PY - 2021 IS - 4 SN - 2075-163X DO - 10.3390/min11040417 UR - https://m2.mtmt.hu/api/publication/31977502 ID - 31977502 LA - English DB - MTMT ER - TY - JOUR AU - Motte, G AU - Hoareau, G AU - Callot, JP AU - Révillon, S AU - Piccoli, F AU - Calassou, S AU - Gaucher, EC. TI - Rift and salt-related multi-phase dolomitization: example from the northwestern Pyrenees JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 126 PY - 2021 PG - 28 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2021.104932 UR - https://m2.mtmt.hu/api/publication/31829006 ID - 31829006 LA - English DB - MTMT ER - TY - JOUR AU - Raucsikné Varga, Andrea Beáta TI - Karbonátkristályok a "Pannon-tenger alól": a mélység mámora ásványtani megközelítésben JF - GEODA J2 - GEODA VL - 31 PY - 2021 IS - 1 SP - 32 EP - 36 PG - 5 SN - 2060-212X UR - https://m2.mtmt.hu/api/publication/31931781 ID - 31931781 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Xiong, Y AU - Wang, LC AU - Tan, XC AU - Liu, Yun AU - Liu, MJ AU - Qiao, ZF TI - Dolomitization of the Ordovician subsalt Majiagou Formation in the central Ordos Basin, China: fluid origins and dolomites evolution JF - PETROLEUM SCIENCE J2 - PETROL SCI VL - 18 PY - 2021 SP - 362 EP - 379 PG - 18 SN - 1672-5107 DO - 10.1007/s12182-020-00522-1 UR - https://m2.mtmt.hu/api/publication/31674311 ID - 31674311 LA - English DB - MTMT ER - TY - JOUR AU - Fintor, Krisztián AU - Raucsikné Varga, Andrea Beáta TI - Paleofluid Fingerprint as an Independent Paleogeographic Correlation Tool: An Example from Pennsylvanian Sandstones and Neighboring Crystalline Rocks (Tisia Composite Terrane, S Hungary) JF - GEOFLUIDS J2 - GEOFLUIDS VL - 2020 PY - 2020 PG - 24 SN - 1468-8115 DO - 10.1155/2020/3568986 UR - https://m2.mtmt.hu/api/publication/31253429 ID - 31253429 N1 - Funding Agency and Grant Number: University of Szeged Open Access Fund [4389]; Bolyai Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences [BO/266/18]; National Research, Development and Innovation Fund [OTKA K 108375]; New National Excellence Program of the Ministry of Human Capacities [UNKP-18-4-SZTE-16]; New National Excellence Program of the Ministry for Innovation and Technology [UNKP-19-4-SZTE-34] Funding text: For petrographic analysis of the Pennsylvanian Teseny rocks, Mining and Geological Survey of Hungary (Dept. of Geological and Geophysical Collections, Budapest) provided thin section collection from borehole Bm-1. We thank Gyorgy Szakmany and Sandor Jozsa (Eotvos Lorand University, Budapest), Zoltan Mathe (Mecsekerc Ltd., Pecs), and Balint Peterdi (Mining and Geological Survey of Hungary) for the studied samples. The authors are grateful to Tivadar M. Toth (University of Szeged) and Ronald J. Bakker and Federica Zaccarrini (Montanuniversitat Leoben) for their supports during analytical measurements. This work was financially supported by the University of Szeged Open Access Fund (4389), the Bolyai Research Scholarship of the Hungarian Academy of Sciences (BO/266/18), the National Research, Development and Innovation Fund (OTKA K 108375), the New National Excellence Program of the Ministry of Human Capacities (UNKP-18-4-SZTE-16), and the New National Excellence Program of the Ministry for Innovation and Technology (UNKP-19-4-SZTE-34). LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Hips, Kinga TI - A rejtelmes dolomit JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 150 PY - 2020 IS - 2 SP - 233 EP - 266 PG - 34 SN - 0015-542X DO - 10.23928/foldt.kozl.2020.150.2.233 UR - https://m2.mtmt.hu/api/publication/31372620 ID - 31372620 N1 - Cited By :1 Export Date: 4 January 2023 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Jiao, X AU - Liu, Y AU - Yang, W AU - Zhou, D AU - Bai, B AU - Zhang, T AU - Zhao, M AU - Li, Z AU - Meng, Z AU - Yang, Y AU - Li, Z TI - Fine-grained volcanic-hydrothermal sedimentary rocks in Permian Lucaogou Formation, Santanghu Basin, NW China: Implications on hydrocarbon source rocks and accumulation in lacustrine rift basins JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 114 PY - 2020 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2019.104201 UR - https://m2.mtmt.hu/api/publication/31034402 ID - 31034402 LA - English DB - MTMT ER - TY - JOUR AU - Kolchugin, A AU - Immenhauser, A AU - Morozov, V AU - Walter, B AU - Eskin, A AU - Korolev, E AU - Neuser, R TI - A comparative study of two Mississippian dolostone reservoirs in the Volga-Ural Basin, Russia JF - JOURNAL OF ASIAN EARTH SCIENCES J2 - J ASIAN EARTH SCI VL - 199 PY - 2020 SN - 1367-9120 DO - 10.1016/j.jseaes.2020.104465 UR - https://m2.mtmt.hu/api/publication/31355707 ID - 31355707 LA - English DB - MTMT ER - TY - THES AU - Li, X TI - Evaluating the Effects of Carbonate Saturation State on Carbonate Platform Geometry and Porosity Evolution - A Case Study from the Great Bank of Guizhou of South China PB - Stanford University PY - 2020 SN - 9798662511651 UR - https://m2.mtmt.hu/api/publication/34518926 ID - 34518926 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 - 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 - THES AU - Lukoczki, G TI - Geochemistry and Crystal Structure of Recrystallized Dolomites PB - Oklahoma State University PY - 2019 SN - 9781392783535 UR - https://m2.mtmt.hu/api/publication/34449714 ID - 34449714 LA - English DB - MTMT ER - TY - JOUR AU - Lukoczki, Georgina AU - Haas, János AU - Gregg, JM AU - Machel, HG AU - Kele, Sándor AU - John, CM TI - Multi-phase dolomitization and recrystallization of Middle Triassic shallow marine–peritidal carbonates from the Mecsek Mts. (SW Hungary), as inferred from petrography, carbon, oxygen, strontium and clumped isotope data JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 101 PY - 2019 SP - 440 EP - 458 PG - 19 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2018.12.004 UR - https://m2.mtmt.hu/api/publication/30342399 ID - 30342399 N1 - Funding Agency and Grant Number: American Association of Petroleum Geologists; Geological Society of America Graduate Student Research Grant Program; International Association of Sedimentologists; Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [OTKA K124313]; National Research, Development and Innovation Office (NKFIH) [KH 125584] Funding text: This work was supported by the American Association of Petroleum Geologists Grants-in-Aid Program, the Geological Society of America Graduate Student Research Grant Program, the International Association of Sedimentologists Post-Graduate Grant Scheme, and the Hungarian Scientific Research Fund (OTKA K124313). SK was supported by the National Research, Development and Innovation Office (NKFIH, KH 125584). The authors are indebted to Tames Budai and Gyula Konrad for their continued help and support, and to Mecsekerc Ltd. for providing access to the VP-2 drill cores. The comments and suggestions of Alessandro Iannace and an anonymous reviewer are greatly appreciated. This is an Oklahoma State University Boone Pickens School of Geology contribution #2018-93. LA - English DB - MTMT ER - TY - JOUR AU - Raucsikné Varga, Andrea Beáta AU - Bozsó, Gábor AU - Garaguly, István AU - Raucsik, Béla AU - Bencsik, Attila AU - Kóbor, Balázs TI - Cements, Waters, and Scales: An Integrated Study of the Szeged Geothermal Systems (SE Hungary) to Characterize Natural Environmental Conditions of the Thermal Aquifer JF - GEOFLUIDS J2 - GEOFLUIDS VL - 2019 PY - 2019 PG - 21 SN - 1468-8115 DO - 10.1155/2019/4863814 UR - https://m2.mtmt.hu/api/publication/30644307 ID - 30644307 N1 - Department of Mineralogy Geochemistry and Petrology, University of SzegedH-6722, Hungary Geothermal Service Provider LtdH-6724, Hungary Export Date: 27 November 2019 Correspondence Address: Varga, A.; Department of Mineralogy Geochemistry and Petrology, University of SzegedHungary; email: raucsikvarga@geo.u-szeged.hu Funding Agency and Grant Number: Economy Development and Innovation Operative Programme [GINOP-2.1.1-15-2016-00970]; National Research, Development and Innovation Fund of Hungary [K 108375] Funding text: The authors are thankful for the hydrochemical data and the scale and rock samples from the geothermal heating systems operating in Szeged owned by the Geothermal Service Provider Ltd., Hungary. This research was financially supported by the Economy Development and Innovation Operative Programme (GINOP-2.1.1-15-2016-00970). Regarding sandstone reservoir characterization, this research was also supported by the National Research, Development and Innovation Fund of Hungary (project Number K 108375). LA - English DB - MTMT ER -