@article{MTMT:34568349,
	title = {Spatiotemporal distribution of magmatism and crustal inheritance within an extensional–rotational environment : an updated geochronology of the Miocene and Quaternary magmatism of the South Apuseni Mountains},
	url = {https://m2.mtmt.hu/api/publication/34568349},
	author = {Ene, VV and Tapster, S and Smith, DJ and Panaiotu, C and Roșu, E and Naden, J and Munteanu, M},
	doi = {10.1144/jgs2023-048},
	journal-iso = {J GEOL SOC LONDON},
	journal = {JOURNAL OF THE GEOLOGICAL SOCIETY},
	volume = {181},
	unique-id = {34568349},
	issn = {0016-7649},
	abstract = {Extension-related magmatism with arc-like features was active in the South Apuseni Mountains, Romania during the Neogene and Quaternary. The current chronological framework is primarily restricted to K–Ar dates. We present here new laser ablation inductively coupled plasma mass spectrometry U–Pb zircon age data for 20 subvolcanic and volcanic rocks from eight different Cenozoic volcanic–intrusive complexes and from Jurassic and Cretaceous lava flows. Our results support magmatic ages between c. 14 and c. 7 Ma, with Uroi, an alkaline intrusion, occurring significantly later at c. 1.5 Ma. Revising the timeline for the South Apuseni Mountains palaeomagnetic rotations shows that most of the clockwise vertical-axis rotation of these mountains (54.4° ± 10.7°) took place between c. 14 and 11 Ma, the age interval when the majority of the magmas were emplaced. Xenocrystic zircon dates show differences in the age populations between individual volcanic–intrusive complexes. A Permo-Triassic population is almost ubiquitous, indicating that basement Permo-Triassic igneous rocks are more widespread than previously thought, or that they were significantly involved in the generation of Neogene magmas. However, other observed age populations, such as Triassic or Paleogene, have no clear correspondence in the known geological record, indicating the presence of a cryptic component interacting with Neogene magmas.},
	year = {2024},
	eissn = {2041-479X},
	orcid-numbers = {Ene, VV/0009-0007-2722-8979; Tapster, S/0000-0001-9049-0485; Smith, DJ/0000-0002-8685-7886; Panaiotu, C/0000-0001-9332-8926; Naden, J/0000-0003-3097-5530}
}

@article{MTMT:34643332,
	title = {Iron-Bearing Minerals in the Boda Claystone Formation: Correspondences with Stages of Evolution Revealed by Mössbauer Spectroscopy},
	url = {https://m2.mtmt.hu/api/publication/34643332},
	author = {Lázár, Károly and Máthé, Z and Németh, Tibor and Kovácsné Kis, Viktória and Stichleutner, Sándor and Kovács, Ivett},
	doi = {10.3390/min14020196},
	journal-iso = {MINERALS-BASEL},
	journal = {MINERALS},
	volume = {14},
	unique-id = {34643332},
	year = {2024},
	eissn = {2075-163X},
	orcid-numbers = {Németh, Tibor/0000-0002-1836-6006; Kovács, Ivett/0000-0001-7015-7909}
}

@article{MTMT:34272140,
	title = {Provenance of far-traveled nappes in the eastern Mediterranean (Uppermost Unit, Crete): constraints from U–Pb zircon ages of detrital and igneous zircons},
	url = {https://m2.mtmt.hu/api/publication/34272140},
	author = {Zulauf, G. and Dörr, W. and Albert, R. and Martha, SO. and Xypolias, P.},
	doi = {10.1007/s00531-023-02356-9},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {113},
	unique-id = {34272140},
	issn = {1437-3254},
	abstract = {New U–Pb ages of detrital and igneous zircons of the Uppermost Unit of Crete shed light on its provenance and on Eohellenic to Eoalpine imprints in the eastern Mediterranean. The detrital zircons of all nappes show Variscan ages and are characterized by a Minoan-type age spectrum, which is typical for the NE margin of Gondwana. Parts of the metasedimentary rocks are unexpectedly young. Their detrital zircon ages continue via the Permian until the Late Triassic, Middle Jurassic and Early Cretaceous. The high-grade metamorphic rocks of the Asterousia crystalline complex are likely equivalents of the low-grade metamorphic trench and fore-arc deposits of the Vatos nappe pointing to Late Cretaceous slab roll back. The presence of both late Permian detrital zircons and Late Cretaceous arc-type granitoids suggest that the Uppermost Unit of Crete is derived from the late Permian/Late Cretaceous magmatic belt situated north of the Sava–Vardar–Izmir–Ankara Suture in the Strandja–Rhodope area. To achieve their recent position on Crete, the nappes had to travel more than 500 km. The traveling path is well tracked by rocks of the Upper Cycladic Unit, which are similar to those of the Uppermost Unit of Crete. The large displacement of the Cretan nappes was controlled not only by nappe transport, but probably also by dextral strike–slip along the North Anatolian Fault Zone and related counterclockwise rotation of the Anatolian block since the Eocene.},
	year = {2024},
	eissn = {1437-3262},
	pages = {23-47},
	orcid-numbers = {Zulauf, G./0000-0002-6483-7614}
}

@article{MTMT:33801573,
	title = {Petrological, mineralogical and geochemical studies of Late Ediacaran A-type Volcanics, North Arabian Shield, Saudi Arabia},
	url = {https://m2.mtmt.hu/api/publication/33801573},
	author = {Abd Allah, SE and Elwan, WI and Abu Anbar, MM and Azzaz, SAD and Alrashidi, KN and El-Awady, A},
	doi = {10.21608/bfszu.2022.158040.1174},
	journal-iso = {Bulletin of Faculty of Science, Zagazig University},
	journal = {Bulletin of Faculty of Science, Zagazig University},
	volume = {2023},
	unique-id = {33801573},
	year = {2023},
	eissn = {1110-1555},
	pages = {32-66}
}

@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:32869078,
	title = {The anorogenic late Ediacaran granite-rhyolite porphyries of Gabal Abu Durba, Sinai: termination of magmatism in the Neoproterozoic Arabian-Nubian Shield crust},
	url = {https://m2.mtmt.hu/api/publication/32869078},
	author = {El-Bialy, MZ. and Zoheir, BA. and Koutsovitis, P and Feigenson, M and Omar, MM.},
	doi = {10.1080/00206814.2022.2079009},
	journal-iso = {INT GEOL REV},
	journal = {INTERNATIONAL GEOLOGY REVIEW},
	volume = {65},
	unique-id = {32869078},
	issn = {0020-6814},
	year = {2023},
	eissn = {1938-2839},
	pages = {843-882},
	orcid-numbers = {Koutsovitis, P/0000-0003-3580-2196}
}

@article{MTMT:33126810,
	title = {Origin, timing and paleogeographic implications of Paleogene karst bauxites in the northern Transdanubian range, Hungary},
	url = {https://m2.mtmt.hu/api/publication/33126810},
	author = {Kelemen, Péter and Dunkl, István and Csillag, Gábor and Mindszenty, Andrea and Józsa, Sándor and Fodor, László and von Eynatten, Hilmar},
	doi = {10.1007/s00531-022-02249-3},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {112},
	unique-id = {33126810},
	issn = {1437-3254},
	abstract = {Paleogene karst bauxites in the northeastern Transdanubian Range and their cover sequences provide valuable sedimentary archives, despite their weathered nature and vague paleontological records. U–Pb detrital zircon geochronology combined with heavy mineral analysis indicates ‘local’ Alpine aeolian and fluvial sources and ‘distant’ aeolian sources connected to the Bohemian Massif. Records of episodic Paleogene volcanic eruptions related to igneous complexes of the Adamello and probably also the Bergell, Recsk and Balkan Peninsula, are reflected by euhedral zircon crystals. Their U–Pb geochronology supplies age constraints for the phases of subaerial exposure of the karstic surface and the accumulation of bauxitic protoliths and helps to improve the existing stratigraphic records and to define stages of denudation in the northeastern Transdanubian Range. Distinct phases of subaerial exposure and accumulation of the bauxite's protoliths are identified as ca. 42, 35 and 31 Ma; alternating with episodes of subsidence, represented by siliciclastic and carbonatic sequences at ca. 38, 32 and 31 Ma. Besides Paleogene volcanism, zircon dating also revealed contributions from the Middle Triassic tuffs of the Transdanubian Range. Garnet, epidote, kyanite, staurolite, and xenotime/monazite crystals suggest fluvial drainage of diverse metamorphic units of the Austroalpine basement from the Eastern- and Southern Alps, which also supplied most of the pre-Mesozoic zircons. However, the unexpectedly high proportion of Variscan ages in the bauxites most likely relate to igneous rocks of the Bohemian Massif, thus suggesting additional long-distance aeolian sources. The new data allow for detailed reconstructions of the Paleogene evolution and palaeogeography of the northeastern Transdanubian range.},
	year = {2023},
	eissn = {1437-3262},
	pages = {243-264},
	orcid-numbers = {Mindszenty, Andrea/0000-0001-8927-3053; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:34104768,
	title = {Large-volume Permian felsic volcanism in the Tisza Mega-unit (East-Central Europe): Evidence from mineralogy, petrology, geochemistry, and geochronology},
	url = {https://m2.mtmt.hu/api/publication/34104768},
	author = {Szemerédi, Máté and Raucsikné Varga, Andrea Beáta and Haranginé Lukács, Réka and Dunkl, István and Seghedi, I and Tatu, M and Kovács, Zoltán and Raucsik, Béla and Benkó, Zsolt and Harangi, Szabolcs and Pál-Molnár, Elemér},
	doi = {10.1016/j.lithos.2023.107330},
	journal-iso = {LITHOS},
	journal = {LITHOS},
	volume = {456-457},
	unique-id = {34104768},
	issn = {0024-4937},
	year = {2023},
	eissn = {1872-6143},
	orcid-numbers = {Szemerédi, Máté/0000-0002-7432-8418; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Haranginé Lukács, Réka/0000-0002-2338-4209; Raucsik, Béla/0000-0002-1951-5974; Harangi, Szabolcs/0000-0003-2372-4581; Pál-Molnár, Elemér/0000-0002-9606-0133}
}

@article{MTMT:33926162,
	title = {Clarification of the Lopingian palaeoclimatic conditions of the northwestern coastal regions of Palaeotethys based on the Transdanubian geological record},
	url = {https://m2.mtmt.hu/api/publication/33926162},
	author = {Trájer, Attila János},
	doi = {10.1016/j.revpalbo.2023.104917},
	journal-iso = {REV PALAEOBOT PALYNO},
	journal = {REVIEW OF PALAEOBOTANY AND PALYNOLOGY},
	volume = {16},
	unique-id = {33926162},
	issn = {0034-6667},
	year = {2023},
	eissn = {1879-0615},
	orcid-numbers = {Trájer, Attila János/0000-0003-3248-6474}
}

@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:33535625,
	title = {Geochronology, geochemistry, and geodynamic evolution of Tatric granites from crystallization to exhumation (Tatra Mountains, Western Carpathians)},
	url = {https://m2.mtmt.hu/api/publication/33535625},
	author = {Catlos, EJ. and Broska, I and Kohút, M and Etzel, TM. and Kyle, JR and Stockli, DF. and Miggins, DP and Campos, D},
	doi = {10.31577/GeolCarp.73.6.1},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {73},
	unique-id = {33535625},
	issn = {1335-0552},
	year = {2022},
	eissn = {1336-8052},
	pages = {517-544},
	orcid-numbers = {Catlos, EJ./0000-0001-6043-3498; Broska, I/0000-0002-8464-8976; Kohút, M/0000-0001-5749-4732; Etzel, TM./0000-0002-8593-718X; Kyle, JR/0000-0002-5319-8941; Stockli, DF./0000-0001-7652-2129; Miggins, DP/0000-0001-8256-8377}
}

@article{MTMT:32826574,
	title = {Permian-Triassic granites of the Schladming complex (Austroalpine basement): Implications for subduction of the Paleo-Tethys Ocean in the Eastern Alps},
	url = {https://m2.mtmt.hu/api/publication/32826574},
	author = {Huang, Q and Neubauer, F and Liu, Y and Genser, J and Guan, Q and Chang, R and Yuan, S and Yu, S},
	doi = {10.1016/j.gr.2022.05.006},
	journal-iso = {GONDWANA RES},
	journal = {GONDWANA RESEARCH},
	volume = {109},
	unique-id = {32826574},
	issn = {1342-937X},
	year = {2022},
	eissn = {1878-0571},
	pages = {205-224}
}

@inproceedings{MTMT:33112456,
	title = {Új kőzettani és geokémiai eredmények a nyugat-mecseki miocén Szászvári Formációban előforduló vulkáni eredetű kőzettörmelékekről (Gyűrűfűi Lapillitufa Formáció)},
	url = {https://m2.mtmt.hu/api/publication/33112456},
	author = {Máthé, Árpád and Miklós, Dóra Georgina and Szemerédi, Máté and Török, Kálmán and Máthé, Zoltán and Józsa, Sándor},
	booktitle = {Calce et malleo – Mésszel és kalapáccsal},
	unique-id = {33112456},
	year = {2022},
	pages = {98-101},
	orcid-numbers = {Miklós, Dóra Georgina/0009-0009-1774-8510; Szemerédi, Máté/0000-0002-7432-8418; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:32787530,
	title = {Permian A-type rhyolites of the Drienok Nappe, Inner Western Carpathians, Slovakia: Tectonic setting from in-situ zircon U-Pb LA-ICP-MS dating},
	url = {https://m2.mtmt.hu/api/publication/32787530},
	author = {Ondrejka, M and Vojtko, R and Putis, M and Chew, DM. and Olsavsky, M and Uher, P and Nemec, O and Drakou, F and Molnárová, A and Spisiak, J},
	doi = {10.31577/GeolCarp.73.2.2},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {73},
	unique-id = {32787530},
	issn = {1335-0552},
	keywords = {rhyolite; Permian; LA-ICP-MS zircon U-Pb dating; Drienok Nappe},
	year = {2022},
	eissn = {1336-8052},
	pages = {123-136}
}

@article{MTMT:33023842,
	title = {Origin and timing of spilitic alterations in volcanic rocks from Głuszyca Górna in the Intra-Sudetic Basin, Poland},
	url = {https://m2.mtmt.hu/api/publication/33023842},
	author = {Powolny, T and Dumańska-Słowik, M and Anczkiewicz, AA. and Sikorska-Jaworowska, M},
	doi = {10.1038/s41598-022-15644-2},
	journal-iso = {SCI REP},
	journal = {SCIENTIFIC REPORTS},
	volume = {12},
	unique-id = {33023842},
	issn = {2045-2322},
	year = {2022},
	eissn = {2045-2322}
}

@{MTMT:33094441,
	title = {Late Paleozoic igneous episodes in the Pannonian Basin and the Apuseni Mts: petrology, zircon U–Pb dating, and regional correlations},
	url = {https://m2.mtmt.hu/api/publication/33094441},
	author = {Szemerédi, Máté and Raucsikné Varga, Andrea Beáta and Haranginé Lukács, Réka and Dunkl, István and Seghedi, I. and Tatu, M. and Kovács, Zoltán and Szepesi, János and Józsa, Sándor and Raucsik, Béla and Harangi, Szabolcs and Jákri, B. and Máthé, Á. and Pál-Molnár, Elemér},
	booktitle = {XXII International Congress of the Carpathian-Balkan Geological Association (CBGA)},
	unique-id = {33094441},
	year = {2022},
	pages = {99-99},
	orcid-numbers = {Szemerédi, Máté/0000-0002-7432-8418; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Haranginé Lukács, Réka/0000-0002-2338-4209; Józsa, Sándor/0000-0001-8219-0044; Raucsik, Béla/0000-0002-1951-5974; Harangi, Szabolcs/0000-0003-2372-4581; Pál-Molnár, Elemér/0000-0002-9606-0133}
}

@mastersthesis{MTMT:33212508,
	title = {A Tiszai-főegység (Tisia-megaterrénum) paleozoos aljzati képződményeinek regionális korrelációja reprezentatív mélyfúrási szelvények felhasználásával},
	url = {https://m2.mtmt.hu/api/publication/33212508},
	author = {Raucsikné Varga, Andrea Beáta},
	unique-id = {33212508},
	year = {2022},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482}
}

@article{MTMT:32075619,
	title = {Paleogeographic implications of a multi-parameter Paleogene provenance dataset (Transylvanian Basin, Romania)},
	url = {https://m2.mtmt.hu/api/publication/32075619},
	author = {Obbágy, Gabriella and Dunkl, István and Józsa, Sándor and Silye, Lóránd and Arató, Róbert and Lünsdorf, NK and von Eynatten, H},
	doi = {10.2110/jsr.2020.080},
	journal-iso = {J SEDIMENT RES},
	journal = {JOURNAL OF SEDIMENTARY RESEARCH},
	volume = {91},
	unique-id = {32075619},
	issn = {1527-1404},
	year = {2021},
	eissn = {1938-3681},
	pages = {551-570},
	orcid-numbers = {Józsa, Sándor/0000-0001-8219-0044; Silye, Lóránd/0000-0001-7306-6041}
}

@article{MTMT:32080577,
	title = {Permian A-type granites of the Western Carpathians and Transdanubian regions: products of the Pangea supercontinent breakup},
	url = {https://m2.mtmt.hu/api/publication/32080577},
	author = {Ondrejka, M and Uher, P and Putiš, M and Kohút, M and Broska, I and Larionov, A and Bojar, AV and Sobocký, T},
	doi = {10.1007/s00531-021-02064-2},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {110},
	unique-id = {32080577},
	issn = {1437-3254},
	year = {2021},
	eissn = {1437-3262},
	pages = {2133-2155},
	orcid-numbers = {Ondrejka, M/0000-0003-1021-5761; Putiš, M/0000-0003-2529-3762; Kohút, M/0000-0001-5749-4732; Broska, I/0000-0002-8464-8976; Bojar, AV/0000-0002-5266-1754}
}

@article{MTMT:31983637,
	title = {The possible source of uranium mineralization in felsic volcanic rocks, Eastern Desert, Egypt of the Arabian-Nubian Shield: Constraints from whole-rock geochemistry and spectrometric prospection},
	url = {https://m2.mtmt.hu/api/publication/31983637},
	author = {Saleh, GM. and Emad, BM. and Kader, IBA and Sakr, RM.},
	doi = {10.1007/s11631-021-00472-4},
	journal-iso = {ACTA GEOCHIM},
	journal = {ACTA GEOCHIMICA},
	volume = {40},
	unique-id = {31983637},
	issn = {2096-0956},
	year = {2021},
	eissn = {2365-7499},
	pages = {819-845}
}

@article{MTMT:32558406,
	title = {Petrology and zircon U–Pb dating of granitoid rocks in the Highiş massif (SW Apuseni Mts., Romania): Insights into Permian plutonic–volcanic connections},
	url = {https://m2.mtmt.hu/api/publication/32558406},
	author = {Szemerédi, Máté and Raucsikné Varga, Andrea Beáta and Dunkl, I. and Haranginé Lukács, Réka and Seghedi, I. and Kovács, Zoltán and Raucsik, Béla and Pál-Molnár, Elemér},
	doi = {10.31577/GeolCarp.72.6.3},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {72},
	unique-id = {32558406},
	issn = {1335-0552},
	year = {2021},
	eissn = {1336-8052},
	pages = {482-504},
	orcid-numbers = {Szemerédi, Máté/0000-0002-7432-8418; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Haranginé Lukács, Réka/0000-0002-2338-4209; Raucsik, Béla/0000-0002-1951-5974; Pál-Molnár, Elemér/0000-0002-9606-0133}
}

@{MTMT:32185048,
	title = {A Zempléni-egység permokarbon összletének korrelációs jelentősége},
	url = {https://m2.mtmt.hu/api/publication/32185048},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla},
	booktitle = {Átalakulások II.},
	unique-id = {32185048},
	year = {2021},
	pages = {59-62},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974}
}

@article{MTMT:31833702,
	title = {Thermal history of the southern Central Cordillera and its exhumation record in the Cenozoic deposits of the Upper Magdalena Valley, Colombia},
	url = {https://m2.mtmt.hu/api/publication/31833702},
	author = {Villamizar-Escalante, N. and Bernet, M. and Urueña-Suárez, C. and Hernández-González, J.S. and Terraza-Melo, R. and Roncancio, J. and Muñoz-Rocha, J.A. and Peña-Urueña, M.L. and Amaya, S. and Piraquive, A.},
	doi = {10.1016/j.jsames.2020.103105},
	journal-iso = {J S AM EARTH SCI},
	journal = {JOURNAL OF SOUTH AMERICAN EARTH SCIENCES},
	volume = {107},
	unique-id = {31833702},
	issn = {0895-9811},
	year = {2021},
	eissn = {1873-0647}
}

@article{MTMT:31911961,
	title = {Evidence for widespread mid-Permian magmatic activity related to rifting following the Variscan orogeny (Western Carpathians)},
	url = {https://m2.mtmt.hu/api/publication/31911961},
	author = {Villaseñor, G and Catlos, EJ. and Broska, I and Kohút, M and Hraško, Ľ and Aguilera, K and Etzel, TM. and Kyle, JR and Stockli, DF.},
	doi = {10.1016/j.lithos.2021.106083},
	journal-iso = {LITHOS},
	journal = {LITHOS},
	volume = {390-391},
	unique-id = {31911961},
	issn = {0024-4937},
	year = {2021},
	eissn = {1872-6143}
}

@article{MTMT:32543737,
	title = {U–Pb zircon ages from Permian volcanites of the Čierna Hora Mts. (Western Carpathians, Slovakia): Regional tectonic implications},
	url = {https://m2.mtmt.hu/api/publication/32543737},
	author = {Vozárová, A and Rodionov, N and Šarinová, K and Vozár, J},
	doi = {10.31577/GeolCarp.72.5.1},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {72},
	unique-id = {32543737},
	issn = {1335-0552},
	year = {2021},
	eissn = {1336-8052},
	pages = {361-372},
	orcid-numbers = {Rodionov, N/0000-0001-5201-1922; Šarinová, K/0000-0003-1792-5862}
}

@article{MTMT:31596016,
	title = {Lavas or ignimbrites? Permian felsic volcanic rocks of the Tisza Mega-unit (SE Hungary) revisited. A petrographic study},
	url = {https://m2.mtmt.hu/api/publication/31596016},
	author = {Szemerédi, Máté and Raucsikné Varga, Andrea Beáta and Szepesi, János and Pál-Molnár, Elemér and Haranginé Lukács, Réka},
	doi = {10.1556/24.2020.00003},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {63},
	unique-id = {31596016},
	issn = {1788-2281},
	year = {2020},
	eissn = {1789-3348},
	pages = {1-18},
	orcid-numbers = {Szemerédi, Máté/0000-0002-7432-8418; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Pál-Molnár, Elemér/0000-0002-9606-0133; Haranginé Lukács, Réka/0000-0002-2338-4209}
}

@{MTMT:31596978,
	title = {Variszkuszi granitoidok a Tiszai-főegységben: új cirkon U–Pb-koradatok},
	url = {https://m2.mtmt.hu/api/publication/31596978},
	author = {Szemerédi, Máté and Pál-Molnár, Elemér and Dunkl, István and Haranginé Lukács, Réka},
	booktitle = {Átalakulások},
	unique-id = {31596978},
	year = {2020},
	pages = {81-81},
	orcid-numbers = {Szemerédi, Máté/0000-0002-7432-8418; Pál-Molnár, Elemér/0000-0002-9606-0133; Haranginé Lukács, Réka/0000-0002-2338-4209}
}

@mastersthesis{MTMT:31836563,
	title = {Results of the complex analyses of the Gyűrűfű Rhyolite Formation in the Tisza Mega-unit (Hungary) [A Gyűrűfűi Riolit Formáció komplex vizsgálati eredményei a Tiszai-főegységben]},
	url = {https://m2.mtmt.hu/api/publication/31836563},
	isbn = {9798381069051},
	author = {Szemerédi, Máté},
	doi = {10.14232/phd.10580},
	publisher = {SZTE},
	unique-id = {31836563},
	keywords = {ignimbrite; rhyolite; Permian; lava; Whole-rock geochemistry; Zircon U-Pb},
	year = {2020},
	orcid-numbers = {Szemerédi, Máté/0000-0002-7432-8418}
}

@book{MTMT:31409086,
	title = {Geokémia olvasóleckék},
	url = {https://m2.mtmt.hu/api/publication/31409086},
	author = {Raucsikné Varga, Andrea Beáta},
	publisher = {SZTE TTIK Ásványtani, Geokémiai és Kőzettani Tanszék},
	unique-id = {31409086},
	year = {2020},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482}
}

@article{MTMT:31664722,
	title = {Widespread Permian granite magmatism in Lower Austroalpine units: significance for Permian rifting in the Eastern Alps},
	url = {https://m2.mtmt.hu/api/publication/31664722},
	author = {Yuan, S and Neubauer, F and Liu, Y and Genser, J and Liu, B and Yu, S and Chang, R and Guan, Q},
	doi = {10.1186/s00015-020-00371-5},
	journal-iso = {SWISS J GEOSCI},
	journal = {SWISS JOURNAL OF GEOSCIENCES},
	volume = {113},
	unique-id = {31664722},
	issn = {1661-8726},
	year = {2020},
	eissn = {1661-8734}
}

@{MTMT:30843796,
	title = {Láva vagy ignimbrit? Átalakult és felülírt szövetek permi savanyú vulkáni kőzetekből (DK-Magyarország, Tiszai-főegység, Békés-Codru szerkezeti öv)},
	url = {https://m2.mtmt.hu/api/publication/30843796},
	author = {Szemerédi, Máté and Raucsikné Varga, Andrea Beáta and Szepesi, János and Pál-Molnár, Elemér and Haranginé Lukács, Réka},
	booktitle = {Saxa Loquuntur - Kőbe zárt történetek},
	unique-id = {30843796},
	year = {2019},
	pages = {81-82},
	orcid-numbers = {Szemerédi, Máté/0000-0002-7432-8418; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Pál-Molnár, Elemér/0000-0002-9606-0133; Haranginé Lukács, Réka/0000-0002-2338-4209}
}

@inproceedings{MTMT:30843798,
	title = {Magmás gránátok: kulcsszerep a Tisia permi Si-gazdag vulkanitjainak petrogenetikájában?},
	url = {https://m2.mtmt.hu/api/publication/30843798},
	author = {Szemerédi, Máté and Vígh, Csaba and Haranginé Lukács, Réka and Raucsikné Varga, Andrea Beáta and Seghedi, I. and Pál-Molnár, Elemér and Dunkl, István and Fehér, K. and Harangi, Szabolcs},
	booktitle = {Saxa Loquuntur - Kőbe zárt történetek},
	unique-id = {30843798},
	year = {2019},
	pages = {82-85},
	orcid-numbers = {Szemerédi, Máté/0000-0002-7432-8418; Haranginé Lukács, Réka/0000-0002-2338-4209; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Pál-Molnár, Elemér/0000-0002-9606-0133; Harangi, Szabolcs/0000-0003-2372-4581}
}

@mastersthesis{MTMT:31272557,
	title = {Zircon dating and trace element content of transparent heavy minerals in sandstones from the NE Alps and Outer Dinarides flysch basins},
	url = {https://m2.mtmt.hu/api/publication/31272557},
	author = {Velicogna, M},
	publisher = {University of Trieste},
	unique-id = {31272557},
	year = {2019}
}