@book{MTMT:33825476,
	title = {Magyarország litosztratigráfiai egységeinek leírása I.. Prekainozoos képződmények},
	url = {https://m2.mtmt.hu/api/publication/33825476},
	isbn = {9789636713287},
	editor = {Babinszki, Edit and Piros, Olga and Budai, Tamás and Gyalog, László and Halász, Amadé and Király, Edit and Koroknai, B and Haranginé Lukács, Réka and M. Tóth, Tivadar},
	publisher = {Supervisory Authority for Regulatory Affairs},
	unique-id = {33825476},
	year = {2023},
	orcid-numbers = {Halász, Amadé/0000-0003-4582-8883; Haranginé Lukács, Réka/0000-0002-2338-4209; M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:33594461,
	title = {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},
	url = {https://m2.mtmt.hu/api/publication/33594461},
	author = {Raucsikné Varga, Andrea Beáta and Pál-Molnár, Elemér and Raucsik, Béla},
	doi = {10.1155/2023/8600576},
	journal-iso = {GEOFLUIDS},
	journal = {GEOFLUIDS},
	volume = {2023},
	unique-id = {33594461},
	issn = {1468-8115},
	abstract = {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.},
	year = {2023},
	eissn = {1468-8123},
	pages = {1-18},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Pál-Molnár, Elemér/0000-0002-9606-0133; Raucsik, Béla/0000-0002-1951-5974}
}

@article{MTMT:34053465,
	title = {Lacustrine Shale Diagenesis—A Case Study of the Second Member of the Funing Formation in the Subei Basin},
	url = {https://m2.mtmt.hu/api/publication/34053465},
	author = {Wang, S and Ma, C and Sun, X and Liu, S},
	doi = {10.3390/pr11072009},
	journal-iso = {PROCESSES},
	journal = {PROCESSES},
	volume = {11},
	unique-id = {34053465},
	issn = {2227-9717},
	abstract = {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.},
	keywords = {Shale; pore evolution; Diagenetic process; diagenetic sequence; Diagenesis types},
	year = {2023},
	eissn = {2227-9717}
}

@article{MTMT:33538610,
	title = {A DOM regulation model for dolomite versus calcite precipitation in the Ediacaran ocean: Implications for the “dolomite problem”},
	url = {https://m2.mtmt.hu/api/publication/33538610},
	author = {Wang, W and Li, C and Dodd, MS. and Algeo, TJ. and Zhang, Z and Cheng, M and Hou, M},
	doi = {10.1016/j.precamres.2022.106947},
	journal-iso = {PRECAMBRIAN RES},
	journal = {PRECAMBRIAN RESEARCH},
	volume = {385},
	unique-id = {33538610},
	issn = {0301-9268},
	keywords = {carbon stable isotopes; dissolved organic matter; Ediacaran age; Doushantuo formation; DOUNCE; Ocean stratification; Shuram Excursion},
	year = {2023},
	eissn = {1872-7433}
}

@article{MTMT:34011869,
	title = {Magnesium isotope trace dolomitization fluid migration path: A case study of the Carboniferous Huanglong Formation in the Sichuan basin},
	url = {https://m2.mtmt.hu/api/publication/34011869},
	author = {Zhu, G and Li, X and Li, T and Zhou, L and Wu, Y and Shen, B and Ning, M},
	doi = {10.19762/j.cnki.dizhixuebao.2022057},
	journal-iso = {ACTA GEOLOGICA SINICA},
	journal = {ACTA GEOLOGICA SINICA},
	volume = {97},
	unique-id = {34011869},
	issn = {0001-5717},
	keywords = {dolomitization; SICHUAN BASIN; Magnesium isotopes; Carboniferous; Huanglong Formation},
	year = {2023},
	pages = {753-771}
}

@article{MTMT:34181718,
	title = {Progress in genetic types and research methods of dolomite},
	url = {https://m2.mtmt.hu/api/publication/34181718},
	author = {Zhu, G and Li, X},
	doi = {10.7623/syxb202307012},
	journal-iso = {Shiyou Xuebao/Acta Petrolei Sinica},
	journal = {Shiyou Xuebao/Acta Petrolei Sinica},
	volume = {44},
	unique-id = {34181718},
	issn = {0253-2697},
	year = {2023},
	pages = {1167-1190}
}

@article{MTMT:32771241,
	title = {How fluid-mediated rock transformations can mimic hydro-fracturing patterns in hydrothermal dolomite},
	url = {https://m2.mtmt.hu/api/publication/32771241},
	author = {Centrella, S and Beaudoin, NE. and Koehn, D and Motte, G and Hoareau, G and Callot, JP},
	doi = {10.1016/j.marpetgeo.2022.105657},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {140},
	unique-id = {32771241},
	issn = {0264-8172},
	keywords = {recrystallization; modelling; breccia; hydrothermal dolomite},
	year = {2022},
	eissn = {1873-4073},
	orcid-numbers = {Beaudoin, NE./0000-0002-7027-8599; Koehn, D/0000-0002-2276-2626}
}

@article{MTMT:32823659,
	title = {Multiple fluid flow events and diversity of hydrothermal minerals in Neoproterozoic to lower Paleozoic carbonate reservoirs, Tarim Basin, NW China},
	url = {https://m2.mtmt.hu/api/publication/32823659},
	author = {Li, K and Cai, C and Tan, X and Jiang, H and Fan, J},
	doi = {10.1016/j.jseaes.2022.105260},
	journal-iso = {J ASIAN EARTH SCI},
	journal = {JOURNAL OF ASIAN EARTH SCIENCES},
	volume = {233},
	unique-id = {32823659},
	issn = {1367-9120},
	keywords = {carbonate; fluid inclusion; TARIM BASIN; Hydrothermal; Neoproterozoic; Stable oxygen and carbon isotopes; Stable Sr isotopes},
	year = {2022},
	eissn = {1878-5786}
}

@article{MTMT:33098794,
	title = {Unraveling overprinted formation mechanisms of massive dolostone in the Lower Triassic sequence of an isolated carbonate platform in Nanpanjiang Basin, south China},
	url = {https://m2.mtmt.hu/api/publication/33098794},
	author = {Li, X and Lehrmann, DJ. and Luczaj, J and Kelley, BM. and Cantrell, DL. and Yu, M and Ferrill, NL and Payne, JL.},
	doi = {10.1016/j.sedgeo.2022.106240},
	journal-iso = {SEDIMENT GEOL},
	journal = {SEDIMENTARY GEOLOGY},
	volume = {440},
	unique-id = {33098794},
	issn = {0037-0738},
	keywords = {REFLUX; Early Triassic; CARBONATE PLATFORM; BURIAL; dolomitization},
	year = {2022},
	eissn = {1879-0968}
}

@article{MTMT:32533869,
	title = {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)},
	url = {https://m2.mtmt.hu/api/publication/32533869},
	author = {Noorian, Y and Moussavi-Harami, R and Hollis, C and Reijmer, JJG. and Mahboubi, A and Omidpour, A},
	doi = {10.1016/j.sedgeo.2021.106048},
	journal-iso = {SEDIMENT GEOL},
	journal = {SEDIMENTARY GEOLOGY},
	volume = {427},
	unique-id = {32533869},
	issn = {0037-0738},
	keywords = {Sequence stratigraphy; Asmari formation; Seepage reflux dolomitization; Porosity evolution; Sabkha},
	year = {2022},
	eissn = {1879-0968}
}

@article{MTMT:32737944,
	title = {Extensive recrystallization of Cenozoic dolomite during shallow burial: A case study from the Palaeocene–Eocene Umm er Radhuma formation and a global meta-analysis},
	url = {https://m2.mtmt.hu/api/publication/32737944},
	author = {Ryan, BH and Kaczmarek, SE and Rivers, JM and Manche, CJ},
	doi = {10.1111/sed.12982},
	journal-iso = {SEDIMENTOLOGY},
	journal = {SEDIMENTOLOGY},
	volume = {69},
	unique-id = {32737944},
	issn = {0037-0746},
	abstract = {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.},
	year = {2022},
	eissn = {1365-3091},
	pages = {2053-2079}
}

@article{MTMT:32106701,
	title = {Reflux dolomitization and subsequent hydrothermal dolomitization induced by the Alkaline Igneous Province in the Middle Devonian Nowshera Formation (Peshawar Basin, NW Pakistan)},
	url = {https://m2.mtmt.hu/api/publication/32106701},
	author = {Ahmad, W and Ullah, S and Ahmad, I and Gingras, MK. and Shafique, M and Khan, EU and Shah, Mumtaz},
	doi = {10.1016/j.marpetgeo.2021.105178},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {131},
	unique-id = {32106701},
	issn = {0264-8172},
	keywords = {Seepage reflux dolomitization; isotopic signature; Magmatic fluid; saddle dolomite; Peshawar Basin; Peshawar Plain Alkaline Igneous Province},
	year = {2021},
	eissn = {1873-4073},
	orcid-numbers = {Ahmad, W/0000-0002-0251-764X; Khan, EU/0000-0002-3748-2811}
}

@article{MTMT:32089112,
	title = {U-pb dating and geochemical constraints to early cretaceous hydrothermal dolomitization in the provenÇal domain (Maritime alps, nw italy-se france)},
	url = {https://m2.mtmt.hu/api/publication/32089112},
	author = {Barale, L. and Bertok, C. and D’atri, A. and Piana, F. and Bernasconi, S.M. and Czuppon, György and Palcsu, László and Gerdes, A. and Birgel, D. and Martire, L.},
	doi = {10.4454/ofioliti.v46i2.543},
	journal-iso = {OFIOLITI},
	journal = {OFIOLITI},
	volume = {46},
	unique-id = {32089112},
	issn = {0391-2612},
	year = {2021},
	pages = {131-149},
	orcid-numbers = {Czuppon, György/0000-0002-7231-6042}
}

@article{MTMT:31933741,
	title = {Structure, genesis and resources efficiency of dolomite: New insights and remaining enigmas},
	url = {https://m2.mtmt.hu/api/publication/31933741},
	author = {Cai, WK and Liu, JH and Zhou, CH and Keeling, J and Glasmacher, UA.},
	doi = {10.1016/j.chemgeo.2021.120191},
	journal-iso = {CHEM GEOL},
	journal = {CHEMICAL GEOLOGY},
	volume = {573},
	unique-id = {31933741},
	issn = {0009-2541},
	year = {2021},
	eissn = {1872-6836}
}

@article{MTMT:31876066,
	title = {Hydrothermal Fluid Activity and Its Reformation on Reservoirs in Qikou Depression},
	url = {https://m2.mtmt.hu/api/publication/31876066},
	author = {Hou, Z. and Zhou, L. and Jin, F. and Chen, S. and Pu, X. and Yan, J. and Li, H.},
	doi = {10.3799/dqkx.2019.282},
	journal-iso = {EARTH SCI J CHINA UNIV GEOSCI},
	journal = {DIQIU KEXUE / EARTH SCIENCE: JOURNAL OF CHINA UNIVERSITY OF GEOSCIENCES},
	volume = {46},
	unique-id = {31876066},
	issn = {1000-2383},
	year = {2021},
	pages = {200-214}
}

@article{MTMT:31977502,
	title = {Re–Os and Sr Isotopic Study of Permian–Triassic Sedimentary Rocks from the Himalaya: Shale Chronology and Carbonate Diagenesis},
	url = {https://m2.mtmt.hu/api/publication/31977502},
	author = {Mandal, A and Tripathy, GR and Goswami, V and Ackerman, L and Parcha, SK. and Chandra, R},
	doi = {10.3390/min11040417},
	journal-iso = {MINERALS-BASEL},
	journal = {MINERALS},
	volume = {11},
	unique-id = {31977502},
	year = {2021},
	eissn = {2075-163X},
	orcid-numbers = {Mandal, A/0000-0002-1884-9542; Ackerman, L/0000-0001-6330-1482}
}

@article{MTMT:31829006,
	title = {Rift and salt-related multi-phase dolomitization: example from the northwestern Pyrenees},
	url = {https://m2.mtmt.hu/api/publication/31829006},
	author = {Motte, G and Hoareau, G and Callot, JP and Révillon, S and Piccoli, F and Calassou, S and Gaucher, EC.},
	doi = {10.1016/j.marpetgeo.2021.104932},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {126},
	unique-id = {31829006},
	issn = {0264-8172},
	year = {2021},
	eissn = {1873-4073}
}

@article{MTMT:31931781,
	title = {Karbonátkristályok a "Pannon-tenger alól": a mélység mámora ásványtani megközelítésben},
	url = {https://m2.mtmt.hu/api/publication/31931781},
	author = {Raucsikné Varga, Andrea Beáta},
	journal-iso = {GEODA},
	journal = {GEODA},
	volume = {31},
	unique-id = {31931781},
	issn = {2060-212X},
	year = {2021},
	pages = {32-36},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482}
}

@article{MTMT:31674311,
	title = {Dolomitization of the Ordovician subsalt Majiagou Formation in the central Ordos Basin, China: fluid origins and dolomites evolution},
	url = {https://m2.mtmt.hu/api/publication/31674311},
	author = {Xiong, Y and Wang, LC and Tan, XC and Liu, Yun and Liu, MJ and Qiao, ZF},
	doi = {10.1007/s12182-020-00522-1},
	journal-iso = {PETROL SCI},
	journal = {PETROLEUM SCIENCE},
	volume = {18},
	unique-id = {31674311},
	issn = {1672-5107},
	year = {2021},
	eissn = {1995-8226},
	pages = {362-379}
}

@article{MTMT:31253429,
	title = {Paleofluid Fingerprint as an Independent Paleogeographic Correlation Tool: An Example from Pennsylvanian Sandstones and Neighboring Crystalline Rocks (Tisia Composite Terrane, S Hungary)},
	url = {https://m2.mtmt.hu/api/publication/31253429},
	author = {Fintor, Krisztián and Raucsikné Varga, Andrea Beáta},
	doi = {10.1155/2020/3568986},
	journal-iso = {GEOFLUIDS},
	journal = {GEOFLUIDS},
	volume = {2020},
	unique-id = {31253429},
	issn = {1468-8115},
	year = {2020},
	eissn = {1468-8123},
	orcid-numbers = {Fintor, Krisztián/0000-0003-4794-9419; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482}
}

@article{MTMT:31372620,
	title = {A rejtelmes dolomit},
	url = {https://m2.mtmt.hu/api/publication/31372620},
	author = {Haas, János and Hips, Kinga},
	doi = {10.23928/foldt.kozl.2020.150.2.233},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {150},
	unique-id = {31372620},
	issn = {0015-542X},
	year = {2020},
	eissn = {2559-902X},
	pages = {233-266},
	orcid-numbers = {Haas, János/0000-0003-0929-8889; Hips, Kinga/0000-0003-2315-120X}
}

@article{MTMT:31034402,
	title = {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},
	url = {https://m2.mtmt.hu/api/publication/31034402},
	author = {Jiao, X and Liu, Y and Yang, W and Zhou, D and Bai, B and Zhang, T and Zhao, M and Li, Z and Meng, Z and Yang, Y and Li, Z},
	doi = {10.1016/j.marpetgeo.2019.104201},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {114},
	unique-id = {31034402},
	issn = {0264-8172},
	year = {2020},
	eissn = {1873-4073}
}

@article{MTMT:31355707,
	title = {A comparative study of two Mississippian dolostone reservoirs in the Volga-Ural Basin, Russia},
	url = {https://m2.mtmt.hu/api/publication/31355707},
	author = {Kolchugin, A and Immenhauser, A and Morozov, V and Walter, B and Eskin, A and Korolev, E and Neuser, R},
	doi = {10.1016/j.jseaes.2020.104465},
	journal-iso = {J ASIAN EARTH SCI},
	journal = {JOURNAL OF ASIAN EARTH SCIENCES},
	volume = {199},
	unique-id = {31355707},
	issn = {1367-9120},
	keywords = {HYDROCARBONS; Russia; dolomite; diagenesis; CARBONATE RESERVOIR; Mississippian; Volga-Ural Basin},
	year = {2020},
	eissn = {1878-5786},
	orcid-numbers = {Kolchugin, A/0000-0002-0959-5085}
}

@mastersthesis{MTMT:34518926,
	title = {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},
	url = {https://m2.mtmt.hu/api/publication/34518926},
	isbn = {9798662511651},
	author = {Li, X},
	publisher = {Stanford University},
	unique-id = {34518926},
	year = {2020}
}

@article{MTMT:31614407,
	title = {Lithologically controlled behaviour of the Dorozsma metamorphic hydrocarbon reservoir (Pannonian Basin, SE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/31614407},
	author = {M. Tóth, Tivadar and Vargáné Tóth, I},
	doi = {10.1016/j.petrol.2020.107748},
	journal-iso = {J PETROL SCI ENG},
	journal = {JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING},
	volume = {195},
	unique-id = {31614407},
	issn = {0920-4105},
	year = {2020},
	eissn = {1873-4715},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:31646840,
	title = {Localisation of Ancient Migration Pathways inside a Fractured Metamorphic Hydrocarbon Reservoir in South-East Hungary},
	url = {https://m2.mtmt.hu/api/publication/31646840},
	author = {M. Tóth, Tivadar and Molnár, László and Körmös, Sándor and Czirbus, Nóra and Schubert, Félix},
	doi = {10.3390/app10207321},
	journal-iso = {APPL SCI-BASEL},
	journal = {APPLIED SCIENCES-BASEL},
	volume = {10},
	unique-id = {31646840},
	keywords = {Pannonian Basin; DFN modelling; FRACTURED RESERVOIRS; Well-logs; Fluid inclusion chemostratigraphy},
	year = {2020},
	eissn = {2076-3417},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Körmös, Sándor/0000-0003-4439-6804; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:30852034,
	title = {Results, problems and future tasks of palaeostress and fault-slip analyses in the Pannonian Basin: the Hungarian contribution},
	url = {https://m2.mtmt.hu/api/publication/30852034},
	author = {Fodor, László},
	doi = {10.23928/foldt.kozl.2019.149.4.297},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {149},
	unique-id = {30852034},
	issn = {0015-542X},
	year = {2019},
	eissn = {2559-902X},
	pages = {297-326}
}

@mastersthesis{MTMT:34449714,
	title = {Geochemistry and Crystal Structure of Recrystallized Dolomites},
	url = {https://m2.mtmt.hu/api/publication/34449714},
	isbn = {9781392783535},
	author = {Lukoczki, G},
	publisher = {Oklahoma State University},
	unique-id = {34449714},
	year = {2019}
}

@article{MTMT:30342399,
	title = {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},
	url = {https://m2.mtmt.hu/api/publication/30342399},
	author = {Lukoczki, Georgina and Haas, János and Gregg, JM and Machel, HG and Kele, Sándor and John, CM},
	doi = {10.1016/j.marpetgeo.2018.12.004},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {101},
	unique-id = {30342399},
	issn = {0264-8172},
	keywords = {Stable Isotope; palaeogeography; Middle Triassic; Mecsek Mts.; dolomitization; clumped isotope},
	year = {2019},
	eissn = {1873-4073},
	pages = {440-458},
	orcid-numbers = {Lukoczki, Georgina/0000-0002-0661-0198; Haas, János/0000-0003-0929-8889; Kele, Sándor/0000-0002-8607-7636; John, CM/0000-0001-9711-1548}
}

@article{MTMT:30644307,
	title = {Cements, Waters, and Scales: An Integrated Study of the Szeged Geothermal Systems (SE Hungary) to Characterize Natural Environmental Conditions of the Thermal Aquifer},
	url = {https://m2.mtmt.hu/api/publication/30644307},
	author = {Raucsikné Varga, Andrea Beáta and Bozsó, Gábor and Garaguly, István and Raucsik, Béla and Bencsik, Attila and Kóbor, Balázs},
	doi = {10.1155/2019/4863814},
	journal-iso = {GEOFLUIDS},
	journal = {GEOFLUIDS},
	volume = {2019},
	unique-id = {30644307},
	issn = {1468-8115},
	year = {2019},
	eissn = {1468-8123},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Garaguly, István/0000-0002-2802-0738; Raucsik, Béla/0000-0002-1951-5974}
}