TY - JOUR AU - Segesdi, Martin AU - Ősi, Attila TI - Sauropterygian remains from the Middle Triassic of Villány, Hungary—new information on the aquatic reptile fauna of Tisza Megaunit (Triassic southern Eurasian shelf region) JF - PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS J2 - PALAEOBIODIV PALAEOENV VL - 101 PY - 2021 IS - 4 SP - 985 EP - 1011 PG - 27 SN - 1867-1594 DO - 10.1007/s12549-020-00480-x UR - https://m2.mtmt.hu/api/publication/31904372 ID - 31904372 N1 - Funding Agency and Grant Number: Eotvos Lorand University; Human Capacities Grant Management Office (EMET) of the Hungarian Ministry of Human Capacities [NTP-NFTO-16-0257]; National Research, Development and Innovation Office-NKFIH [OTKA K 116665, K 131597]; ELTE Dinosaur Research Group Funding text: Open Access funding provided by Eotvos Lorand University. Research was funded by the Human Capacities Grant Management Office (EMET) of the Hungarian Ministry of Human Capacities (M. Segesdi-NTP-NFTO-16-0257; National Talent Support Program Scholarship), the National Research, Development and Innovation Office-NKFIH (A. Osi-OTKA K 116665, K 131597) and the ELTE Dinosaur Research Group. LA - English DB - MTMT ER - TY - JOUR AU - Lazăr, Iuliana AU - Schlagintweit, Felix AU - Grădinaru, Eugen TI - Halorina cryptica nov. ichnogen., nov. ichnosp., mass-occurrence of Upper Triassic crustacean microcoprolites from neptunian dikes and sills cutting the Dachstein-type carbonate platform and their paleoenvironmental significance (Northern Apuseni Mountains, Romania) JF - GEOBIOS J2 - GEOBIOS-LYON VL - 61 PY - 2020 SP - 31 EP - 39 PG - 9 SN - 0016-6995 DO - 10.1016/j.geobios.2020.06.003 UR - https://m2.mtmt.hu/api/publication/31382822 ID - 31382822 N1 - Department of Geology, Faculty of Geology and Geophysics, University of Bucharest, 1 N. Bălcescu Bd, Bucharest, 010041, Romania Lerchenauerstr. 167, München, 80935, Germany Cited By :1 Export Date: 26 August 2022 Correspondence Address: Lazăr, I.; Department of Geology, 1 N. Bălcescu Bd, Romania; email: iuliana.lazar@g.unibuc.ro 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 - Early dolomitization and partial burial recrystallization: a case study of Middle Triassic peritidal dolomites in the Villány Hills (SW Hungary) using petrography, carbon, oxygen, strontium and clumped isotope data JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 109 PY - 2020 IS - 3 SP - 1051 EP - 1070 PG - 20 SN - 1437-3254 DO - 10.1007/s00531-020-01851-7 UR - https://m2.mtmt.hu/api/publication/31270514 ID - 31270514 N1 - Funding Agency and Grant Number: American Association of Petroleum Geologists; Geological Society of America Graduate Student Research Grant Program; International Association of Sedimentologists Post-Graduate Grant Scheme; Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [OTKA K124313]; National Research, Development and Innovation Office (NKFIH, Hungary) [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 (Grant number OTKA K124313). SK was supported by the National Research, Development and Innovation Office (NKFIH, Hungary) (Grant number KH 125584). The authors are indebted to Tamas Budai, Michael Grammer, Gyula Konrad, James Puckette and Pankaj Sarin for their continued help and support. The comments and suggestions of reviewers Arthur Adams and Oliver Weidlich are greatly appreciated. This is an Oklahoma State University Boone Pickens School of Geology contribution #2020-115. AB - Peritidal carbonates of the Csukma Formation (Csukma Dolomite Member) in the Villany Hills, SW Hungary, were investigated to determine the nature of the dolomitization and recrystallization processes that affected these rocks during their complex tectonic evolution, and to evaluate if clumped isotope data preserved signals from the original dolomitization event or are indicative of the later recrystallization processes. Sedimentary and petrographic features, as well as geochemical characteristics integrated with the tectonic evolution of the area indicate that dolomitization likely occurred penecontemporaneously via geothermal convection of normal-to-slightly modified seawater in a near-surface to shallow burial setting. This was followed by partial recrystallization of the dolomites in an intermediate burial setting with low water-to-rock ratios. Results of this study suggest that the clumped isotope temperatures of dolomites, partially recrystallized via dissolution-re-precipitation, may provide a minimum estimate of the temperature of recrystallization. However, caution has to be taken when interpreting the thermal history and fluid evolution of successions that were affected by significant recrystallization, because the clumped isotope temperatures and the calculated fluid compositions might inaccurately represent the diagenetic conditions. LA - English DB - MTMT ER - TY - JOUR AU - Slovenec, Damir AU - Belak, Mirko AU - Misur, Ivan AU - Segvic, Branimir AU - Schuster, Ralf TI - The early Paleozoic cumulate gabbroic rocks from the southwest part of the Tisza Mega-Unit (Mt. Papuk, NE Croatia): evidence of a Gondwana suture zone JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 109 PY - 2020 IS - 6 SP - 2209 EP - 2233 PG - 25 SN - 1437-3254 DO - 10.1007/s00531-020-01896-8 UR - https://m2.mtmt.hu/api/publication/31422845 ID - 31422845 N1 - Funding Agency and Grant Number: Croatian Ministry of Science, Education and SportMinistry of Science, Education and Sports, Republic of Croatia [181-1951126-1141, 181-1811096-1093]; Croatian Science Foundation [IP-2019-04-3824] Funding text: This work has been supported by the Croatian Ministry of Science, Education and Sport (Grant no. 181-1951126-1141 to Da. S., "Mesozoic magmatic, mantle and pyroclastic rocks of north-western Croatia" and Grant no. 181-1811096-1093 to M. B., Basic Geological Map of Croatia 1:50,000) and in part by the Croatian Science Foundation under the project IP-2019-04-3824. Kevin Byerly is thanked for his assistance with the English language. We are especially in debt to Kalin Kouzmanov (University of Geneva) who has provided the microprobe analyses. Critical comments and constructive reviews by Jurgen von Raumer and one anonymous reviewer, as well as the editorial handling by Jean Francois Moyen and Wolf-Christian Dullo contributed significantly to the manuscript quality. AB - The Mt. Papuk heteroadcumulate pyroxene-amphibole gabbronorites, which outcrops at the southern margin of the Tisza Mega-Unit, is suggested to stem from the deep oceanic crust formed by the in situ crystallisation in a supposed magma chamber. Amphibole oikocrystals are found to define a poikilitic texture of analysed rocks. A common enclosure in amphibole is the cumulus orthopyroxene, and rarely, the clinopyroxene and/or plagioclase and spinel. The chemical composition of related minerals and their crystallisation sequence suggest the sub-solidus crystallisation of gabbronorite in an open system at high temperatures and medium pressures. Parental magmas originated from the moderately depleted mantle source, which was metasomatised prior to melting. Early mineral fractionation gave rise to the assemblage consisted of spinel, pyroxene, plagioclase and intercumulus amphibole. The rocks' bulk chemistry, mineral crystallisation sequence, pyroxene geochemistry and myriad of high Ca-plagioclase, which coexists with igneous Ca-amphibole are all in favour of the strong subduction influence typical for mafic intrusion formed above mantle wedge in the root of an island arc at depths of 10-21 km. Herein presented geochemical and isotopic data (Ar-40-Ar-39: 487.1 +/- 4.3 Ma and Sm-Nd: 505 Ma) go along with the existence of an intra-oceanic arc related to geodynamic events that took place in the Prototethyan oceanic realm s.l. during middle Cambrian to earliest Ordovician. These events were likely correlated with the subduction of the Quaidam(?) back-arc ocean, or alternatively, with the subduction and closure of Prototethyan branches located between microcontinental fragments of Asia. Initially, the closure of back-arc oceans led to crust fragmentation and, then, addition of non-metamorphosed mafites into the obducted sequence further from the active continental margins of Gondwana and Laurassia at the time of the formation of Pangea in the late Palaeozoic. 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 - Szabó, Márton AU - Botfalvai, Gábor AU - Ősi, Attila TI - Taxonomical and palaeoecological investigations of the chondrichthyan and osteichthyan fish remains from the Middle-Late Triassic deposits of the Villány Hills (Southern Hungary) JF - GEOBIOS J2 - GEOBIOS-LYON VL - 57 PY - 2019 SP - 111 EP - 126 PG - 16 SN - 0016-6995 DO - 10.1016/j.geobios.2019.10.006 UR - https://m2.mtmt.hu/api/publication/30938641 ID - 30938641 N1 - Funding Agency and Grant Number: National Research, Development and Innovation OfficeNational Research, Development & Innovation Office (NRDIO) - Hungary [NKFIH K 116665]; UNKP-19-4 New National Excellence Program of the Ministry for Innovation and Technology [UNKP-19-4-ELTE-117]; Janos Bolyai Research Scholarship of Hungarian Academy of Sciences [BO/00024/19/10]; Hungarian Academy of Sciences Lendulet Program; Hungarian Natural History Museum; Eotvos Lorand University; University of Pecs; Hungarian Dinosaur Foundation Funding text: The authors are grateful to the three reviewers, Gilles Cuny, Guillaume Guinot and Carlo Romano, and to the associate-editor Jeremy Martin for their constructive comments and suggestions that greatly improved an earlier version of the manuscript. We thank Emilia Pozsgai, Krisztina Sebe, Attila Voros, Anette E. Gotz, Istvan Dunkl, Orsolya Gyori, Janos Haas, and Tamas Budai for useful discussions. Reka Kalmar, Janos Magyar and Flora Nemeth are acknowledged for their technical assistance. We thank Krisztina Buczko for her precious help in scanning electron miscroscopic photography. The 2013-2018 field crews are also acknowledged for their enthusiastic assistance in the fieldworks. This work was supported by the National Research, Development and Innovation Office (No: NKFIH K 116665), the UNKP-19-4 New National Excellence Program of the Ministry for Innovation and Technology (No: UNKP-19-4-ELTE-117), the Janos Bolyai Research Scholarship of Hungarian Academy of Sciences (No: BO/00024/19/10), the Hungarian Academy of Sciences Lendulet Program, the Hungarian Natural History Museum, the Eotvos Lorand University, the University of Pecs, and the Hungarian Dinosaur Foundation. LA - English DB - MTMT ER - TY - JOUR AU - Garaguly, István AU - Raucsikné Varga, Andrea Beáta AU - Raucsik, Béla AU - Schubert, Félix AU - Czuppon, György AU - Frei, R TI - Pervasive early diagenetic dolomitization, subsequent hydrothermal alteration, and late stage hydrocarbon accumulation in a Middle Triassic carbonate sequence (Szeged Basin, SE Hungary) JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 98 PY - 2018 SP - 270 EP - 290 PG - 21 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2018.07.024 UR - https://m2.mtmt.hu/api/publication/3399845 ID - 3399845 N1 - Funding Agency and Grant Number: National Research, Development and Innovation Fund of Hungary [K 108375] Funding text: This research was supported by the National Research, Development and Innovation Fund of Hungary (project no. K 108375). The authors would like to thank MOL Plc for providing the core material that were essential for this research. We would like to thank Dr. Fadi H. Nader and the anonymous referee for their suggestions and comments that improve our manuscript, as well as Associated Editor Dr. Ihsan Al-Aasm for the editorial work. Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem utca 2-6, Szeged, 6702, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary Department of Geosciences and Natural Resource Management, University of Copenhagen, ØsterVoldgade10, Copenhagen, 1350, Denmark Nordic Center for Earth Evolution (NordCEE), Copenhagen, Denmark Cited By :15 Export Date: 12 September 2021 Correspondence Address: Garaguly, I.; Department of Mineralogy, Egyetem utca 2-6, Hungary; email: garagulyistvan@gmail.com Funding text 1: This research was supported by the National Research, Development and Innovation Fund of Hungary (project no. K 108375 ). The authors would like to thank MOL Plc for providing the core material that were essential for this research. We would like to thank Dr. Fadi H. Nader and the anonymous referee for their suggestions and comments that improve our manuscript, as well as Associated Editor Dr. Ihsan Al-Aasm for the editorial work. LA - English DB - MTMT ER - TY - JOUR AU - Horvat, M. AU - Klötzli, U. AU - Jamičić, D. AU - Buda, György AU - Klötzli, E. AU - Hauzenberger, C. TI - Geochronology of granitoids from Psunj and Papuk Mts., Croatia JF - GEOCHRONOMETRIA J2 - GEOCHRONOMETRIA VL - 45 PY - 2018 IS - 1 SP - 198 EP - 210 PG - 13 SN - 1733-8387 DO - 10.1515/geochr-2015-0099 UR - https://m2.mtmt.hu/api/publication/30321138 ID - 30321138 N1 - \n Croatian Geological Survey, Department of Geology, Sachsova 2, Zagreb, 10000, Croatia \n University of Vienna, Department of Lithospheric Research, Althanstraße 14, Vienna, A-1090, Austria \n Svetojanska 21, Zagreb, 10000, Croatia \n Eötvös Lóránd University, Institute of Geology, Department of Mineralogy, Pazmany Peter setany 1/c, Budapest, H-1117, Hungary \n Karl-Franzens-University, Department of Earth Sciences, Universitätsplatz 2, Graz, 8010, Austria \n Export Date: 19 November 2018 \n Correspondence Address: Horvat, M.; Croatian Geological Survey, Department of Geology, Sachsova 2, Croatia; email: mhorvat@hgi-cgs.hr Funding Agency and Grant Number: Ministry of Science and Education of the Republic of Croatia; OTKA (Hungarian National Research Fund) [K 67787]; Hungarian Ministry of Education\n Funding text: This work was financed by Ministry of Science and Education of the Republic of Croatia, and supported by OTKA (Hungarian National Research Fund project no. K 67787). The study was carried out partly at the Department of Mineralogy, Eotvos Lorand University, Budapest, and was supported by the Hungarian Ministry of Education through the Ph.D. scholarship of the first author. The study was also carried out at the Department of Geology of the Croatian Geological Survey, as well as at the Department of Lithospheric Research, the University of Vienna, the Department of Earth Sciences, Karl-Franzens-Universitat Graz and the Institute of Applied Geosciences, the Graz Technical University. The authors are very grateful to Livia Rudnyanszky (Department of Mineralogy, Eotvos Lorand University) for zircon separation and Franz Biedermann (Department of Lithospheric Research, University of Vienna) for the preparation of BSE/CL images. The authors would also like to acknowledge Mirko Belak (Department of Geology, Croatian Geological Survey) for useful discussion. Special thanks go to Christian Auer (Geological Survey of Austria, Vienna) for scanning electron microscopy facilities. The authors would like to thank to three anonymous reviewers for their constructive comments, objections and suggestions which have contributed in the reorganization and improvement of the manuscript.\n Funding Agency and Grant Number: Ministry of Science and Education of the Republic of Croatia; OTKA (Hungarian National Research Fund)Orszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [K 67787]; Hungarian Ministry of Education Funding text: This work was financed by Ministry of Science and Education of the Republic of Croatia, and supported by OTKA (Hungarian National Research Fund project no. K 67787). The study was carried out partly at the Department of Mineralogy, Eotvos Lorand University, Budapest, and was supported by the Hungarian Ministry of Education through the Ph.D. scholarship of the first author. The study was also carried out at the Department of Geology of the Croatian Geological Survey, as well as at the Department of Lithospheric Research, the University of Vienna, the Department of Earth Sciences, Karl-Franzens-Universitat Graz and the Institute of Applied Geosciences, the Graz Technical University. The authors are very grateful to Livia Rudnyanszky (Department of Mineralogy, Eotvos Lorand University) for zircon separation and Franz Biedermann (Department of Lithospheric Research, University of Vienna) for the preparation of BSE/CL images. The authors would also like to acknowledge Mirko Belak (Department of Geology, Croatian Geological Survey) for useful discussion. Special thanks go to Christian Auer (Geological Survey of Austria, Vienna) for scanning electron microscopy facilities. The authors would like to thank to three anonymous reviewers for their constructive comments, objections and suggestions which have contributed in the reorganization and improvement of the manuscript. AB - Detailed cathodoluminescence (CL) and back scattered electron (BSE) imaging of zircon crystals, coupled with in-situ U-Pb zircon dating by Laser Ablation Multi-Collector Inductively Coupled Plasma Mass Spectrometry (LA-MC-ICP-MS) were used to develop new insights into the evolution of a monzogranite from Omanovac Quarry (Psunj Mt.), and of monzogranites from Sandrovac Quarry and Kiseljevac Creek (Papuk Mt.), both located in the Slavonian Mountains (Croatia). U-Pb isotopic data yielded a concordia age of 380 +/- 4 Ma for the monzogranite from Omanovac Quarry, and 382 +/- 2 Ma and 383 +/- 5 Ma for monzogranites from Sandrovac Quarry and Kiseljevac Creek. The results suggest Late Devonian magmatic activity. LA - English DB - MTMT ER - TY - JOUR AU - Szurominé, Korecz Andrea AU - Garaguly, István AU - Szente, István AU - Raucsikné Varga, Andrea Beáta AU - Raucsik, Béla TI - „Oázis a sivatagban” — különösen gazdag ősmaradvány-együttes a fosszíliaszegény üllési Szegedi Dolomitból JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 148 PY - 2018 IS - 2 SP - 119 EP - 124 PG - 6 SN - 0015-542X DO - 10.23928/foldt.kozl.2018.148.2.119 UR - https://m2.mtmt.hu/api/publication/3385746 ID - 3385746 N1 - MOL NyRt., Csoportszintű KTD, Alkalmazott Anyagok, Technológiák és Laboratórium, Szent István utca 14, Budapest, Hungary SZTE TTIK Ásványtani, Geokémiai és Kőzettani Tanszék, Egyetem utca 2, Szeged, 6722, Hungary ELTE Tatai Geológus Kert, Pázmány Péter sétány 1/C, Budapest, 1117, Hungary SZTE TTIK ÁGK, “Vulcano” Kőzettani és Geokémiai Kutatócsoport, Egyetem utca 2, Szeged, 6722, Hungary Cited By :2 Export Date: 21 March 2024 Correspondence Address: Garaguly, I.; SZTE TTIK Ásványtani, Egyetem utca 2, Hungary; email: garagulyistvan@gmail.com LA - Hungarian DB - MTMT ER - TY - JOUR AU - Pozsgai, Emília AU - Józsa, Sándor AU - Dunkl, István AU - Sebe, Krisztina AU - Thamóné Bozsó, Edit AU - Sajó, István AU - Dezső, József AU - von Eynatten, H TI - Provenance of the Upper Triassic siliciclastics of the Mecsek Mountains and Villány Hills (Pannonian Basin, Hungary). constraints to the Early Mesozoic paleogeography of the Tisza Megaunit TS - constraints to the Early Mesozoic paleogeography of the Tisza Megaunit JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 106 PY - 2017 IS - 6 SP - 2005 EP - 2024 PG - 20 SN - 1437-3254 DO - 10.1007/s00531-016-1406-0 UR - https://m2.mtmt.hu/api/publication/3132886 ID - 3132886 N1 - Megjegyzés-26917143 Megjegyzés-26809875 OA No Funding Agency and Grant Number: Doctoral School of Earth Sciences of the University Pecs; Szentagothai Research Centre Pecs; Department of Petrology and Geochemistry of the Eotvos Lorand University; Geoscience Centre of the University of Gottingen Funding text: This study was funded by the Doctoral School of Earth Sciences of the University Pecs, Szentagothai Research Centre Pecs, Department of Petrology and Geochemistry of the Eotvos Lorand University, and Geoscience Centre of the University of Gottingen. The authors are grateful to Attila Osi and the Lendulet Dinosaur Research Group for the extended support. We are indebted for the instructions to mineral separation to Irina Ottenbacher (Gottingen), for the photographs and guidance to calculation of chemical composition (SEM) to Kirsten Techmer (Gottingen) and Zsolt Bendo (Budapest), for instructions to Raman spectroscopy to Keno Lunsdorf and Burkhard C. Schmidt (Gottingen) and to XRD to Janos Kovacs (Pecs). We are thankful to Ildiko Havasi (Danube-Drava National Park) for allowing our research at the nature protection area of Templom Hill. We are grateful to Tamas Budai, Akos Halmai, Gyula Konrad, Erzsebet Ralisch-Felgenhauer, Andrea Raucsik-Varga, Tivadar M. Toth and Attila Voros for the constructive discussions. We are grateful to Gabor Tari and Salvatore Critelli for their constructive reviews. AB - The Tisza Megaunit in the Southern Pannonian Basin formed part of the southern margin of the European Plate in the Early Mesozoic era. Its exact paleo-position and relation to other structural blocks is disputed for a long time. Detrital zircon U–Pb dating, heavy mineral analysis and petrographical examination of Carnian to Pliensbachian sandstone members lead to better understanding of the provenance of clastic deposits after the Ladinian–Carnian carbonate to siliciclastic facies shift in the Southwestern Tisza Megaunit. Investigations allow for constraining its paleogeographic relation to adjacent units. The Carnian and Pliensbachian siliciclastics of the Villány Hills derive from inside the Southwestern Tisza Megaunit, i.e. the medium-grade polymetamorphic rocks of the adjacent Slavonian Mountains or similar basement fragments. The Upper Triassic clastic deposits of the Mecsek Mountains most likely derive from Variscan felsic plutonic rocks of the local basement or partially from the Southern/Southwestern Bohemian Massif. About 200 Ma zircon U–Pb ages are tentatively interpreted as traces of synsedimentary distal volcanism in the Central Atlantic Magmatic Province. LA - English DB - MTMT ER - TY - JOUR AU - Baranyi, Viktória AU - Pálfy, József AU - Görög, Ágnes AU - Riding, James B AU - Raucsik, Béla TI - Multiphase response of palynomorphs to the Toarcian Oceanic Anoxic Event (Early Jurassic) in the Réka Valley section, Hungary JF - REVIEW OF PALAEOBOTANY AND PALYNOLOGY J2 - REV PALAEOBOT PALYNO VL - 235 PY - 2016 SP - 51 EP - 70 PG - 20 SN - 0034-6667 DO - 10.1016/j.revpalbo.2016.09.011 UR - https://m2.mtmt.hu/api/publication/3120888 ID - 3120888 N1 - Megjegyzés-26332646 N1 Funding details: K72633, OTKA, Hungarian Scientific Research Fund N1 Funding text: We thank Maria Barbacka (Hungarian Natural History Museum, Budapest), and András Galácz and István Szente (Eötvös Loránd University, Budapest), for their helpful advice. Emese Réka Bodor (Geological and Geophysical Institute of Hungary, Budapest) is thanked for her assistance in the field, and help with data analysis. Elżbieta Witkowska (Jagiellonian University, Kraków, Poland) and Jadwiga Ziaja (Władysław Szafer Institute of Botany, Kraków, Poland) are acknowledged for their help with taxonomy, and for obtaining literature. Emanuela Mattioli (Université Claude Bernard Lyon 1, France) kindly undertook calcareous nannofossil analyses during an earlier project on the section studied. We thank Wolfram M. Kürschner (University of Oslo, Norway) for his constructive comments on an early draft of the manuscript. Two anonymous reviewers provided constructive comments and help in improving this article. The research was financed by the Hungarian Scientific Research Fund (project K72633) and the Hantken Miksa Foundation. Viktória Baranyi was also supported by an AASP Student Scholarship in 2013. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). This is MTM–MTA–ELTE Palaeo contribution number 226. Funding Agency and Grant Number: Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [K72633]; Hantken Miksa Foundation; AASP Student Scholarship; Natural Environment Research CouncilUK Research & Innovation (UKRI)Natural Environment Research Council (NERC) [bgs05002, bgs05016] Funding Source: researchfish Funding text: We thank Maria Barbacka (Hungarian Natural History Museum, Budapest), and Andras Galacz and Istvan Szente (Elitvos Lorand University, Budapest), for their helpful advice. Emese Reka Bodor (Geological and Geophysical Institute of Hungary, Budapest) is thanked for her assistance in the field, and help with data analysis. Elzbieta Witkowska (Jagiellonian University, Krakow, Poland) and Jadwiga Ziaja (Wladyslaw Szafer Institute of Botany, Krakow, Poland) are acknowledged for their help with taxonomy, and for obtaining literature. Emanuela Mattioli (Universite Claude Bernard Lyon 1, France) kindly undertook calcareous nannofossil analyses during an earlier project on the section studied. We thank Wolfram M. Kurschner (University of Oslo, Norway) for his constructive comments on an early draft of the manuscript. Two anonymous reviewers provided constructive comments and help in improving this article. The research was financed by the Hungarian Scientific Research Fund (project K72633) and the Hantken Miksa Foundation. Viktoria Baranyi was also supported by an AASP Student Scholarship in 2013. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). This is MTM-MTA-ELTE Palaeo contribution number 226. AB - Abstract Major palaeoenvironmental and palaeoceanographical changes occurred during the Early Jurassic Toarcian Oceanic Anoxic Event (T-OAE), due to a perturbation of the global carbon cycle and a crisis in marine ecosystems. The sequence of environmental change and regional differences during the T-OAE are not yet fully understood and organic-walled phytoplankton and other palynomorphs are well-suited, but under-utilised, in research into this event. Based on quantitative palynological analyses from a black shale-bearing succession at Réka Valley in the Mecsek Mountains of southwest Hungary, five sequential palynomorph assemblages are distinguished. These reveal major shifts in organic-walled phytoplankton communities, driven by palaeoenvironmental changes. In addition, palynofacies analysis helped to document changes in the composition of sedimentary organic matter, and to quantify the terrestrial input. Assemblage 1 is characterised by a moderately diverse phytoplankton community and high levels of terrestrial palynomorphs. Assemblage 2 records a significant peak of the euryhaline dinoflagellate cyst Nannoceratopsis. Assemblage 3 is distinguished by dominance of highly opportunistic prasinophytes and the temporary disappearance of all dinoflagellate cyst taxa. Assemblages 4 and 5 represent distinctive phases of a prolonged recovery phase with low diversity phytoplankton assemblages and intermittently high levels of terrestrially-derived palynomorphs. The successive disappearance of phytoplankton taxa and the gradual takeover by opportunistic euryhaline species at the onset of the T-OAE were related to several phenomena. These include reduced salinity in the surface waters, establishment of a stable pycnocline and deterioration of nutrient recycling, followed by oxygen deficiency throughout much of the water column. The high amount of terrestrially-derived palynodebris indicates intense runoff and freshwater input, driven by the early Toarcian warming and the enhanced hydrological cycle. Comparison with coeval European successions proves that the palaeoenvironmental changes during the T-OAE were not entirely synchronous, and local factors played a crucial role in influencing phytoplankton communities. In the Mecsek Basin, regional freshening of the surface waters and increased terrestrial input due to the proximity of the hinterland had a greater influence on phytoplankton communities compared to the open oceanic setting of the Tethys to the south. LA - English DB - MTMT ER - TY - CHAP AU - Cəlburean, R AU - Codrea, VA AU - Barbu, O ED - Karadeniz, M ED - Gulsun, Kilic M ED - Torun, Bilgic E ED - Basarir, H ED - Onel, O TI - Opportunities for environmental impact assessment of the geothermal area beiu T2 - 24th International Mining Congress of Turkey, IMCET 2015 PB - TMMOB Maden Mühendisleri Odası CY - Ankara SN - 9786050107050 PB - TMMOB Maden Mühendisleri Odası PY - 2015 SP - 1480 EP - 1485 PG - 6 UR - https://m2.mtmt.hu/api/publication/25316462 ID - 25316462 N1 - A4 Faculty of Economics and Business Administration, Babe-Bolyai University, 58-60 Teodor Mihali Str., Cluj-Napoca, RO-400591, Romania Department of Geology, Faculty of Biology and Geology, Babe-Bolyai University, 1, Kogəlniceanu Str., Cluj-Napoca, RO-400084, Romania Conference code: 112347 Export Date: 15 June 2021 LA - English DB - MTMT ER - TY - CHAP AU - Haas, János ED - Lóczy, Dénes TI - Geological and Tectonic Background T2 - Landscapes and Landforms of Hungary PB - Springer Netherlands CY - Cham SN - 9783319089966 T3 - World Geomorphological Landscapes, ISSN 2213-2090 PY - 2015 SP - 7 EP - 17 PG - 11 DO - 10.1007/978-3-319-08997-3_2 UR - https://m2.mtmt.hu/api/publication/32071291 ID - 32071291 N1 - Cited By :2 Export Date: 15 June 2021 Correspondence Address: Haas, J.; Geological, Pázmány Péter sétány 1/c, Hungary; email: haas@ludens.elte.hu AB - The Pannonian region (the Pannonian or Carpathian Basin and the surrounding mountain ranges) is part of the Mediterranean Mountain System, which was formed during the last plate-tectonic cycle since the latest Paleozoic times. In Europe it is an about 300–800Â km wide belt (Neo-Europe) accreted to the previously consolidated parts of Europe (Hercynian/Variscan Europe or Meso-Europe) as a result of the Alpine orogeny caused by convergence of the European (Eurasian) and African Plates. The present-day geological structure of the region is mostly determined by the evolution of the Tethys and Atlantic Ocean systems, i.e. the dismembering of the European and African continental plate margins during the early evolutionary stages and their tectonic deformation and uplifting as consequences of plate and microplate collisions. Plate-tectonic processes led to the formation of the large Pannonian Basin in the Late Cenozoic times. Hungary lies in the central part of the Pannonian Basin that is actually a system of several basins separated by isolated ranges of Palaeozoic and Mesozoic, sedimentary, magmatic and metamorphic formations and Cenozoic sedimentary and igneous rocks. © 2015, Springer International Publishing Switzerland. LA - English DB - MTMT ER - TY - JOUR AU - Lukoczki, Georgina AU - Budai, Tamás AU - Németh, Tibor TI - Sideritic-kaolinitic and green clay layers in the Mecsek Mountains (SW Hungary): Indicators of Middle Triassic volcanism-myth or reality? JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 58 PY - 2015 IS - 4 SP - 334 EP - 355 PG - 22 SN - 1788-2281 DO - 10.1556/24.58.2015.4.4 UR - https://m2.mtmt.hu/api/publication/3089130 ID - 3089130 N1 - Boone Pickens School of Geology, Oklahoma State University, Stillwater, OK, United States Department of Geology and Meteorology, University of Pécs, Pécs, Hungary Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Pécs, Hungary Geological and Geophysical Institute of Hungary, Budapest, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budapest, Hungary Department of Mineralogy, Eötvös Loránd University, Budapest, Hungary Noble Research Center, Stillwater, OK 74078, United States Cited By :1 Export Date: 28 April 2023 Correspondence Address: Lukoczki, G.; Noble Research CenterUnited States; email: gina.lukoczki@okstate.edu LA - English DB - MTMT ER - TY - JOUR AU - Zajzon, Norbert AU - Szentpéteri, K AU - Szakáll, Sándor AU - Kristály, Ferenc TI - The origin of the Avram Iancu U–Ni–Co–Bi–As mineralization, Ba˘iţa (Bihor) metallogenic district, Bihor Mts., Romania JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 104 PY - 2015 IS - 7 SP - 1865 EP - 1887 PG - 23 SN - 1437-3254 DO - 10.1007/s00531-015-1175-1 UR - https://m2.mtmt.hu/api/publication/2943291 ID - 2943291 LA - English DB - MTMT ER - TY - JOUR AU - Fiser-Nagy, Ágnes AU - Varga-Tóth, I AU - M. Tóth, Tivadar TI - Lithology identification using open-hole well-log data in the metamorphic Kiskunhalas-NE hydrocarbon reservoir, South Hungary JF - ACTA GEODAETICA ET GEOPHYSICA J2 - ACTA GEOD GEOPHYS VL - 49 PY - 2014 IS - 1 SP - 57 EP - 78 PG - 22 SN - 2213-5812 DO - 10.1007/s40328-013-0037-1 UR - https://m2.mtmt.hu/api/publication/2474978 ID - 2474978 AB - in press LA - English DB - MTMT ER - TY - JOUR AU - Hágen, András TI - A monyoródi jura mészkő és miocén konglomerátum feltárás értékelése a földtudományi természetvédelem szempontjából JF - TÁJÖKOLÓGIAI LAPOK / JOURNAL OF LANDSCAPE ECOLOGY J2 - TÁJÖKOLÓGIAI LAPOK / J LANDSCAPE ECOL VL - 12 PY - 2014 IS - 1 SP - 173 EP - 182 PG - 10 SN - 1589-4673 UR - https://m2.mtmt.hu/api/publication/2586947 ID - 2586947 LA - English DB - MTMT ER - TY - JOUR AU - Mercedes-Martín, R AU - Salas, R AU - Arenas, C TI - Microbial-dominated carbonate platforms during the Ladinian rifting: Sequence stratigraphy and evolution of accommodation in a fault-controlled setting (Catalan Coastal Ranges, NE Spain) JF - BASIN RESEARCH J2 - BASIN RES VL - 26 PY - 2014 IS - 2 SP - 269 EP - 296 PG - 28 SN - 0950-091X DO - 10.1111/bre.12026 UR - https://m2.mtmt.hu/api/publication/25316463 ID - 25316463 N1 - Departament de Geoquímica, Petrologia i Prospecció Geològica, Facultat de Geologia, Universitat de Barcelona, C/Martí i Franquès s/n, Barcelona, 08028, Spain Departamento de Ciencias de la Tierra, Área de Estratigrafía, Universidad de Zaragoza, C/Pedro Cerbuna, 12, Zaragoza, 50009, Spain Cited By :10 Export Date: 15 June 2021 Correspondence Address: Mercedes-Martín, R.; Departament de Geoquímica, Petrologia i Prospecció Geològica, Facultat de Geologia, Universitat de Barcelona, C/Martí i Franquès s/n, Barcelona 08028, Spain; email: rmercedes@ub.edu Departament de Geoquímica, Petrologia i Prospecció Geològica, Facultat de Geologia, Universitat de Barcelona, C/Martí i Franquès s/n, Barcelona, 08028, Spain Departamento de Ciencias de la Tierra, Área de Estratigrafía, Universidad de Zaragoza, C/Pedro Cerbuna, 12, Zaragoza, 50009, Spain Cited By :10 Export Date: 21 June 2021 Correspondence Address: Mercedes-Martín, R.; Departament de Geoquímica, Petrologia i Prospecció Geològica, Facultat de Geologia, Universitat de Barcelona, C/Martí i Franquès s/n, Barcelona 08028, Spain; email: rmercedes@ub.edu LA - English DB - MTMT ER - TY - JOUR AU - Chatalov, A TI - A Triassic homoclinal ramp from the Western Tethyan realm, Western Balkanides, Bulgaria: Integrated insight with special emphasis on the Anisian outer to inner ramp facies transition JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 386 PY - 2013 SP - 34 EP - 58 PG - 25 SN - 0031-0182 DO - 10.1016/j.palaeo.2013.04.028 UR - https://m2.mtmt.hu/api/publication/27620817 ID - 27620817 N1 - Megjegyzés-23557272 FN: Thomson Reuters Web of Knowledge Cited By :12 Export Date: 15 June 2021 CODEN: PPPYA Correspondence Address: Chatalov, A.; Department of Mineralogy, 15 Tsar Osvoboditel Bd., BG-1504 Sofia, Bulgaria; email: chatalov@gea.uni-sofia.bg Cited By :12 Export Date: 16 June 2021 CODEN: PPPYA Correspondence Address: Chatalov, A.; Department of Mineralogy, 15 Tsar Osvoboditel Bd., BG-1504 Sofia, Bulgaria; email: chatalov@gea.uni-sofia.bg Cited By :12 Export Date: 17 June 2021 CODEN: PPPYA Correspondence Address: Chatalov, A.; Department of Mineralogy, 15 Tsar Osvoboditel Bd., BG-1504 Sofia, Bulgaria; email: chatalov@gea.uni-sofia.bg Cited By :12 Export Date: 18 June 2021 CODEN: PPPYA Correspondence Address: Chatalov, A.; Department of Mineralogy, 15 Tsar Osvoboditel Bd., BG-1504 Sofia, Bulgaria; email: chatalov@gea.uni-sofia.bg Cited By :12 Export Date: 21 June 2021 CODEN: PPPYA Correspondence Address: Chatalov, A.; Department of Mineralogy, 15 Tsar Osvoboditel Bd., BG-1504 Sofia, Bulgaria; email: chatalov@gea.uni-sofia.bg Cited By :12 Export Date: 30 August 2021 CODEN: PPPYA Correspondence Address: Chatalov, A.; Department of Mineralogy, 15 Tsar Osvoboditel Bd., BG-1504 Sofia, Bulgaria; email: chatalov@gea.uni-sofia.bg LA - English DB - MTMT ER - TY - CHAP AU - Codrea, V AU - Cälburean, R ED - Celik, I. B TI - Geothermal energy in Western Apuseni Mountains (Romania) for economic and sustainable purposes T2 - 23rd International Mining Congress and Exhibition of Turkey, IMCET 2013 PB - Chamber of Mining Engineers of Turkey CY - Antalya SN - 9781632662989 PB - Chamber of Mining Engineers of Turkey PY - 2013 SP - 1707 EP - 1712 PG - 6 UR - https://m2.mtmt.hu/api/publication/25316466 ID - 25316466 N1 - A4 Boren; DEMiR Export; et al; metso Expect results; Outotec; TMMOB Maden Muhendisleri Odasi Boren; DEMiR Export; et al; metso Expect results; Outotec; TMMOB Maden Muhendisleri Odasi Conference code: 105453 Cited By :1 Export Date: 15 June 2021 LA - English DB - MTMT ER - TY - JOUR AU - Császár, Géza AU - Szinger, Balázs AU - Piros, Olga TI - From continental platform towards rifting of the Tisza Unit in the Late Triassic to Early Cretaceous JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 64 PY - 2013 IS - 4 SP - 279 EP - 290 PG - 12 SN - 1335-0552 DO - 10.2478/geoca-2013-0020 UR - https://m2.mtmt.hu/api/publication/2464910 ID - 2464910 N1 - Cited By :7 Export Date: 11 November 2022 Correspondence Address: Eötvös Loránd University, Pazmany Peter setany 1/C, H-1117 Budapest, Hungary Funding details: AT-9/2008, K 68791, T 062468 Funding text 1: Acknowledgments: The study was financially supported by the National Scientific Research Fund T 062468 and K 68791, Fund Aktion Österreich—Ungarn 74öu5 and Fund TéT AT-9/2008. The authors are indebted to Ágnes Görög for her kind help in completing this paper and to the referees for the careful control of the manuscript. AB - The Upper Triassic-Lower Cretaceous successions of the Transdanubian part of the Mecsek and Villany-Bihor Zones of the Tisza Unit have been studied from the lithological, lithostratigraphical, sedimentological, microfossil and microfacies points of view in order to correlate and interpret the significant differences between them and to draw a conclusion about their geological and paleogeographical history. After an overview of the paleogeographical reconstructions of the broader area, the succession of the Mecsek and Villany-Bihor Zones and the debated Mariakemend-Bar Range are introduced. Until the end of the Middle Triassic the study area acted as an entity. The first fundamental difference between the two zones can be recognized in the Late Triassic when marine carbonates were replaced by thick fluvial siliciclastics in the Mecsek Zone, while it is represented only by small, local lenses with a few and thin dolostone intercalations in the Villany Zone. The Mecsek Zone is bordered southward by one of the large listric faults to the north of which very thick siliciclastics developed in the Early to Middle Jurassic, whereas it is highly lacunose in the larger western part of the Villany-Bihor Zone. The break at the base is subaerial, higher in the succession it is shallow submarine. The sediment is silty, occasionally sandy crinoidal limestone of late Early Jurassic or even Middle Jurassic in age. The Upper Jurassic in the Mecsek Zone is composed of deep-water cherty limestone while in the Villany Zone it became a thick, shallowing pelagic limestone with reworked patch reef fragments. It is clear evidence that the Mecsek Zone had a thinned continental crust thanks to the nearby rift zone while in the Villany Zone the crust remained thick. The actualized version of the Plasienka's paleogeographical model (Plasienka 2000) is introduced. LA - English DB - MTMT ER - TY - BOOK ED - Haas, János TI - Geology of Hungary T3 - Regional Geology Reviews ; XXIV. ET - 0 PB - Springer Netherlands CY - Berlin CY - Heidelberg PY - 2013 SP - 236 SN - 3642219098 DO - 10.1007/978-3-642-21910-8 UR - https://m2.mtmt.hu/api/publication/2048748 ID - 2048748 N1 - Geological, Geophysical and Space Science Research Group, Eötvös Loránd University, Budapest, Hungary Geological, Geophysical and Space Science Research Group, Eötvös Loránd University, Budapest, Hungary Cited By :47 Export Date: 1 July 2022 LA - English DB - MTMT ER - TY - JOUR AU - Ősi, Attila AU - Pozsgai, Emília AU - Prondvai, Edina AU - Botfalvai, Gábor AU - Götz, AE AU - Makádi, László AU - Hajdu, ZS AU - Csengődi, D AU - Czirják, G AU - Sebe, Krisztina AU - Szentesi, Zoltán TI - First report of Triassic vertebrate assemblages from the Villány Hills (Southern Hungary) JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 56 PY - 2013 IS - 4 SP - 297 EP - 335 PG - 39 SN - 1788-2281 DO - 10.1556/CEuGeol.56.2013.4.2 UR - https://m2.mtmt.hu/api/publication/2583272 ID - 2583272 LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Budai, Tamás AU - Raucsik, Béla TI - Climatic controls on sedimentary environments in the Triassic of the Transdanubian Range (Western Hungary) JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 353-355 PY - 2012 SP - 31 EP - 44 PG - 14 SN - 0031-0182 DO - 10.1016/j.palaeo.2012.06.031 UR - https://m2.mtmt.hu/api/publication/2048753 ID - 2048753 N1 - Cited By :48 Export Date: 26 August 2022 CODEN: PPPYA Correspondence Address: Raucsik, B.; Department of Geology, Ifjúság útja 6, H-7624 Pécs, Hungary; email: raucsik.bela@gmail.com LA - English DB - MTMT ER - TY - CHAP AU - Haas, János ED - Lóczy, Dénes ED - Stankoviansky, M ED - Kotarba, A TI - Geological and Tectonic setting T2 - Recent landform evolution PB - Springer Netherlands CY - Berlin CY - Heidelberg SN - 9789400724471 T3 - Springer geography PY - 2012 SP - 3 EP - 18 PG - 16 DO - 10.1007/978-94-007-2448-8_1 UR - https://m2.mtmt.hu/api/publication/1982402 ID - 1982402 N1 - Cited By :1 Export Date: 1 July 2022 Correspondence Address: Haas, J.; Department of Geology, Pázmány Péter sétány 1/c, Hungary; email: haas@ludens.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Vörös, Attila TI - Episodic sedimentation on a peri-Tethyan ridge through the Middle-Late Jurassic transition (Villany Mountains, southern Hungary) JF - FACIES J2 - FACIES VL - 58 PY - 2012 IS - 3 SP - 415 EP - 443 PG - 29 SN - 0172-9179 DO - 10.1007/s10347-011-0287-8 UR - https://m2.mtmt.hu/api/publication/2182126 ID - 2182126 N1 - Cited By :17 Export Date: 23 February 2023 Correspondence Address: Vörös, A.; Research Group for Paleontology, , Budapest, Ludovika tér 2, 1083, Hungary; email: voros@nhmus.hu AB - The Villany area, as a central part of the Tisza microcontinent/terrane along the European margin of Tethys, was characterized by intense subsidence in the Early and Middle Triassic, followed by a long interruption of subsidence in the Late Triassic to Middle Jurassic. During the Middle-Late Jurassic transition, marine sedimentation started with three distinct sedimentary episodes dated as Late Bathonian, Early Callovian, and Middle-Late Callovian, respectively. The succession is terminated by a thick limestone of Middle Oxfordian age. The sedimentary features, microfacies, and macroinvertebrate associations of these four stratigraphic units are documented and illustrated. The Middle to Late Jurassic sedimentary episodes of the Villany succession record an interplay of local and global factors and paleogeographical changes. At the beginning, local tectonic movements governed the main features of sedimentation, though the role of eustasy was also essential. From the mid-Callovian onwards, global climatic, biotic, and paleoceanographical changes controlled the nature and formation of the local carbonate sediments. The Callovian stromatolites are attributed to the activity of sulphate-reducing bacteria in a deep sublittoral, current-swept environment. Upwelling of eutrophic Tethyan waters is recorded by the prevalence of the Bositra filament microfacies in the Callovian. The long submarine hiatus at around the Callovian-Oxfordian transition mirrors a serious restriction of the carbonate budget, due to sudden cooling and a change in the oceanic current system (opening of a circumglobal Tethyan Passage), and to a higher amount of dissolved CO2. In the Middle Oxfordian, the carbonate production considerably increased in accordance with the sudden global warming. LA - English DB - MTMT ER - TY - JOUR AU - Posgay, Károly AU - Bodoky, Tamás János AU - Falus, György AU - Kovács, István János AU - Madarasi, András AU - Gúthy, Tibor AU - Hegedűs, Endre AU - Kovács, Attila Csaba TI - Structural formation of Tisza and Száva-Bükk units in the Lower Cretaceous period. A Tisza és a száva-bükki egység szerkezetének alsó-krétabeli alakulása TS - A Tisza és a száva-bükki egység szerkezetének alsó-krétabeli alakulása JF - MAGYAR GEOFIZIKA J2 - MAGYAR GEOFIZIKA VL - 52 PY - 2011 IS - 3 SP - 135 EP - 150 PG - 16 SN - 0025-0120 UR - https://m2.mtmt.hu/api/publication/2030780 ID - 2030780 N1 - Megjegyzés-24492915 Hiányzó Besorolás: 'A Tisza és a száva-bükki egység szerkezetének alsó-krétabeli alakulása',24 Admin megjegyzés-24492915 tblsubtype: (name,DocTypeID) ('A Tisza és a száva-bükki egység szerkezetének alsó-krétabeli alakulása',24) #Besorolás AB - Comparing the deep refl ection seismic profi les (PGT-1, ÉK-2) measured along the Hungarian Geotraverse with geological, magnetotelluric and geochemical data we came to the conclusion that on the surface of the Pre-Cenozoic basement there is a sequence of rocks which is repeated several times along the Geotraverse. That sequence is composed of metamorphic rocks and of Triassic, Jurassic and Cretaceous beds superimposed on them with SSE line of dip and forming belts with SWW-NEE strike. Rows of characteristic refl ections can be observed which are started at the edges of the belts and run along zones of the section sloping towards the SSE part of the profi le. From those dislocation zones can be deduced, which divide the investigated part of Tisza unit into thick plate like blocks. This lithosphere structure might be formed when a branch of the Vardar Ocean (which joined to the Száva-Bükk unit) was pushed under the Tisza unit about during the Lower Cretaceous. The Pre-Cenozoic basement is intersected by the subduction surface along the Mid-Hungarian Line (at least nearby the Hungarian Geotravers). This idea is backed up by the followings: - Those refl ections which are parallel to the dislocation belt starting in the vicinity of the Mid-Hungarian Line and slope towards SSE indicate displacement surfaces. - On the Northern part of the Geotravers (ÉK-2 section) the continuations of these refl ections bend into horizontal direction. From that we may conclude a NNW directional decrease of the sloping of the plate, namely the nearly horizontal part of the plate subducting in SSE direction. - On that upper part of the subducting plate a low resistivity zone revealed by magnetotellurics can be followed to large depth. Presumably this zone sloping SSE indicates a higher water content of the plate which might be bound in chain silicates (amphiboles and micas). The results of our investigation show that on the studied part of the Tisza unit the structure of the thick plate under the flysch is similar to those of its other parts along the Hungarian Geotraverse, namely under the flysch from NNW to SSE crystalline rocks and Triassic, Jurassic and Cretaceous beds superimposed on them can be found. It is conceivable that those layers got into a depth of CH generation protected by flysch. © 2011 Magyar Geofi zikusok Egyesülete. LA - Hungarian DB - MTMT ER - TY - JOUR AU - Siklósy, Zoltán AU - Kern, Zoltán AU - Demény, Attila AU - Pilet, S AU - Leél-Őssy, Szabolcs AU - Lin, K AU - Shen, CC AU - Kovács-Széles, Éva AU - Breitner, Dániel TI - Speleothems and pine trees as sensitive indicators of environmental pollution - A case study of the effect of uranium-ore mining in Hungary JF - APPLIED GEOCHEMISTRY J2 - APPL GEOCHEM VL - 26 PY - 2011 IS - 5 SP - 666 EP - 678 PG - 13 SN - 0883-2927 DO - 10.1016/j.apgeochem.2011.01.025 UR - https://m2.mtmt.hu/api/publication/1537934 ID - 1537934 LA - English DB - MTMT ER - TY - JOUR AU - Kovács, S AU - Buda, György AU - Haas, János AU - Brezsnyánszky, Károly AU - Harangi, Szabolcs TI - Tectonostratigraphic terranes and zones juxtaposed along the Mid-Hungarian Line: their contrasting evolution and relationships JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 53 PY - 2010 IS - 2-3 SP - 165 EP - 180 PG - 16 SN - 1788-2281 DO - 10.1556/CEuGeol.53.2010.2-3.4 UR - https://m2.mtmt.hu/api/publication/1791284 ID - 1791284 N1 - Geological, Geophysicaland Space Science Research Group, HungarianAcademy of Sciences, Budapest, Hungary Eötvös Loránd University, Department of Mineralogy, Budapest, Hungary Geological Institute of Hungary, Budapest Eötvös Loránd University, Department of Petrology and Geochemistry, Budapest, Hungary Pazmany P. setany 1/c, H-1117 Budapest, Hungary Stefánia út 14, H-1143 Budapest, Hungary Cited By :5 Export Date: 5 December 2022 Correspondence Address: Kovács, S.; Geological, Geophysicaland Space Science Research Group, , Budapest, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Petrik, Attila TI - Microtectonic measurements and interpretation of the Mesozoic formations in the Villány Hills and Görcsöny- Máriakéménd Ridge, Hungary JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 53 PY - 2010 IS - 1 SP - 21 EP - 42 PG - 22 SN - 1788-2281 DO - 10.1556/CEuGeol.53.2010.1.2 UR - https://m2.mtmt.hu/api/publication/27640170 ID - 27640170 N1 - Eötvös Lóránd University, Department of Regional Geology, Budapest, Hungary Sárbereki Ltp. 320, H-2800 Tatabánya, Hungary Cited By :3 Export Date: 1 July 2022 Correspondence Address: Petrik, A.; Eötvös Lóránd University, , Budapest, Hungary AB - In the framework of a National Research Fond project varied scientific investigations are being carried out with the aim of preparing a comprehensive paleogeographical reconstruction of the Tisza structural unit. I have joined this project and performed microtectonical measurements in the area of the Villány Hills and Görcsöny- Máriakéménd Ridge. A lot of publications and theses have already been made about the structural development of the Mecsek-Villány area (CSONTOS & BERGERAT 1988; BENKOVICS 1997; CSONTOS ET. AL 2002), but the Villány Hills and their environments were in a shade role contrary to the Mecsek Mountains in them. The task was to establish the delimitation the phases of structural transformation and determine their relative and numeric ages. It has been an important issue to clarify how far the events of structural transformation postulated by me can be integrated into the regional geological processes. The tectonical conditions of the area at issue have been analysed relying upon some stereographical projections, figures and models. In addition describing the structural elements of the 12 quarries investigated in the study demonstrates the related stress fields as well. Seven Villány-, and five Görcsöny- Máriakéménd quarries, the data of over 700 striations, 600 lythoclases, various plastic deformation elements (folds, flexures) as well as stylolites were recorded. It was an important issue to integrate those structural elements into the regional geological processes which didn’t show any significant movements. Based on the data recorded the structural, paleotectonic conditions of the studied area were determined. LA - English DB - MTMT ER - TY - JOUR AU - Vörös, Attila TI - A villányi mezozoos rétegsor: visszatekintés új nézőpontból [The Mesozoic sedimentary sequences at Villány (southern Hungary)] JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 140 PY - 2010 IS - 1 SP - 3 EP - 30 PG - 28 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1417437 ID - 1417437 N1 - Cited By :8 Export Date: 28 April 2023 Correspondence Address: Attila, V.; Magyar Természettudományi Múzeum, Ludovika tér 2, 1083 Budapest, Hungary LA - Hungarian DB - MTMT ER - TY - JOUR AU - Vörös, Attila TI - Tectonically-controlled Late Triassic and Jurassic sedimentary cycles on a peri-Tethyan ridge (Villány, southern Hungary). JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 52 PY - 2009 IS - 2 SP - 125-151 SN - 1788-2281 DO - 10.1556/CEuGeol.52.2009.2.2 UR - https://m2.mtmt.hu/api/publication/1417445 ID - 1417445 N1 - megjelent: 2010-ben LA - English DB - MTMT ER - TY - JOUR AU - Feist-Burkhardt, S AU - Götz, AE AU - Szulc, J AU - Borkhataria, R AU - Geluk, M AU - Haas, János AU - Hornung, J AU - Jordan, P AU - Kempf, O AU - Michalík, J AU - Nawrocki, J AU - Reinhardt, L AU - Ricken, W AU - Röhling, HG AU - Rüffer, T AU - Török, Ákos AU - Zühlke, R TI - Triassic JF - CENTRAL EUROPE J2 - CENTRAL EUROPE VL - 2 PY - 2008 SP - 749 EP - 821 PG - 73 SN - 1479-0963 UR - https://m2.mtmt.hu/api/publication/32550094 ID - 32550094 N1 - Cited By :117 Export Date: 12 January 2023 LA - English DB - MTMT ER - TY - JOUR AU - Palinkas, LA AU - Sostaric, SB AU - Palinkas, SS TI - Metallogeny of the Northwestern and Central Dinarides and Southern Tisia JF - ORE GEOLOGY REVIEWS J2 - ORE GEOL REV VL - 34 PY - 2008 IS - 3 SP - 501 EP - 520 PG - 20 SN - 0169-1368 DO - 10.1016/j.oregeorev.2008.05.006 UR - https://m2.mtmt.hu/api/publication/20754329 ID - 20754329 N1 - FU: Ministry of Sciences, Republic of Croatia [119/098709-1175] FX: We express our sincere gratitude to Franz Neubauer and an anonymous : reviewer for their valuable suggestions which helped us to organize the : text and made the paper more transparent. Thanks go to Nigel Cook, : whose advice helped us clarify the goals of this contribution. Our : gratitude is also assigned to the Ministry of Sciences, Republic of : Croatia, whose financial support of the project No. 119/098709-1175 : enabled preparation of the manuscript. Cited By :27 Export Date: 15 June 2021 Correspondence Address: Palinkaš, L.A.; Faculty of Sciences, Horvatovac bb, 10 000 Zagreb, Croatia; email: lpalinkas@geol.pmf.hr Funding details: Ministarstvo Obrazovanja, Znanosti i Sporta, MZOS, 119/098709-1175 Funding text 1: We express our sincere gratitude to Franz Neubauer and an anonymous reviewer for their valuable suggestions which helped us to organize the text and made the paper more transparent. Thanks go to Nigel Cook, whose advice helped us clarify the goals of this contribution. Our gratitude is also assigned to the Ministry of Sciences, Republic of Croatia, whose financial support of the project No. 119/098709-1175 enabled preparation of the manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Ruckwied, K AU - Götz, A AU - Pálfy, József AU - Török, Ákos TI - Palynology of a terrestrial coal-bearing series across the Triassic/Jurassic boundary (Mecsek Mts, Hungary) JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 51 PY - 2008 IS - 1 SP - 1 EP - 15 PG - 15 SN - 1788-2281 DO - 10.1556/CEuGeol.51.2008.1.1 UR - https://m2.mtmt.hu/api/publication/1247526 ID - 1247526 N1 - Shell International Exploration and Production, Rijswijk, Netherlands Darmstadt University of Technology, Institute of Applied Geosciences, Darmstadt, Germany Hungarian Academy of Sciences, Hungarian Natural History Museum, Research Group for Paleontology, Budapest, Hungary Department of Construction Materials and Engineering Geology, Budapest University of Technology and Economics, Budapest, Hungary Kessler Park 1, NL-2288 GS Rijswijk, Netherlands Schnittspahnstr. 9, D-64287 Darmstadt, Germany P.O. Box 137, H-1431 Budapest, Hungary Sztoczek u. 2, H-1521 Budapest, Hungary Cited By :28 Export Date: 15 June 2021 Correspondence Address: Ruckwied, K.; Shell International Exploration and Production, Rijswijk, Netherlands LA - English DB - MTMT ER - TY - JOUR AU - Schmid, Stefan M AU - Bernoulli, Daniel AU - Fuegenschuh, Bernhard AU - Matenco, Liviu AU - Schefer, Senecio AU - Schuster, Ralf AU - Tischler, Matthias AU - Ustaszewski, Kamil TI - The Alpine-Carpathian-Dinaridic orogenic system: correlation and evolution of tectonic units JF - SWISS JOURNAL OF GEOSCIENCES J2 - SWISS J GEOSCI VL - 101 PY - 2008 IS - 1 SP - 139 EP - 183 PG - 45 SN - 1661-8726 DO - 10.1007/s00015-008-1247-3 UR - https://m2.mtmt.hu/api/publication/25730251 ID - 25730251 N1 - Geologisch-Paläontologisches Institut, Basel University, Bernoullistr. 35, Basel 4058, Switzerland Geology and Palaeontology, Innsbruck University, Innrain 52f, Innsbruck A-6020, Austria Faculty of Earth and Life Sciences, Netherlands Centre for Integrated Solid Earth Sciences, Vrije Universiteit, De Boelelaan 1085, Amsterdam 1081 HV, Netherlands Geologische Bundesanstalt, Neulinggasse 38, Wien A-1030, Austria Cited By :821 Export Date: 15 June 2021 Correspondence Address: Schmid, S. M.; Geologisch-Paläontologisches Institut, Bernoullistr. 35, Basel 4058, Switzerland; email: Stefan.Schmid@unibas.ch Funding details: Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, SNF, 200021-101882/1 Funding text 1: We benefited from a close cooperation with: D. Balen (Zagreb), I. Balin-toni (Cluj), T. Berza (Bucharest), L. Csontos (Budapest), C. Dinu (Bucharest), N. Ðerić (Belgrade), D. Egli (Basel), L. Fodor (Budapest), W. Frank (Vienna), N. Froitzheim (Bonn), H.-J. Gawlick (Leoben), N. Gerzina (Belgrade), F. Horvath (Budapest), H. Hrvatović (Sarajevo), S. Karamata (Belgrade), A. Kounov (Basel), S. Kovács (Budapest), K. Krenn (Graz), C. Legler (Pristina), R. Lein (Vienna), M. Marović (Belgrade), E. Márton (Budapest), K. Onuzi (Tirana), J. Pamić (Zagreb) D. Plašienka (Bratislava), M. Săndulescu (Bucharest), E. Sasaran (Cluj), M. Sudar (Belgrade), V. Schuller (Tübingen), B. Tomljenović (Zagreb) and many others. Clark Burchfiel (Cambridge Mass.) and Peter Ziegler (Binningen) are thanked for their detailed and constructive comments; their reviews substantially improved a first version of the manuscript. Peter Nievergelt finalized the figures. This study was financed through the Swiss National Science Foundation grant Nr. 200021-101882/1 (“Tisza and LA - English DB - MTMT ER - TY - JOUR AU - Hips, Kinga TI - Facies pattern of western Tethyan Middle Triassic black carbonates: The example of Gutenstein Formation in Silica Nappe, Carpathians, Hungary, and its correlation to formations of adjoining areas. JF - SEDIMENTARY GEOLOGY J2 - SEDIMENT GEOL VL - 194 PY - 2007 IS - 1-2 SP - 99 EP - 114 PG - 16 SN - 0037-0738 DO - 10.1016/j.sedgeo.2006.05.001 UR - https://m2.mtmt.hu/api/publication/152181 ID - 152181 N1 - Cited By :19 Export Date: 12 January 2023 Correspondence Address: Hips, K.; Geological Research Group, Pázmány s. 1/c, 1117 Budapest, Hungary; email: hips@ludens.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Posgay, Károly AU - Kovács, Attila Csaba AU - Csabafi, Róbert Imre AU - Bodoky, Tamás János AU - Hegedűs, Endre AU - Fancsik, Tamás AU - Riegler, Balázs TI - A CEL07 mélyszeizmikus szelvény újraértékelése [Reinterpretation of CEL07 deep seismic profile] JF - MAGYAR GEOFIZIKA J2 - MAGYAR GEOFIZIKA VL - 48 PY - 2007 IS - 3 SP - 87 EP - 98 PG - 12 SN - 0025-0120 UR - https://m2.mtmt.hu/api/publication/2247784 ID - 2247784 N1 - Angol összefoglalóval és ábraaláírásokkal LA - Hungarian DB - MTMT ER - TY - JOUR AU - Seghedi, I AU - Bojar, AV AU - Downes, H AU - Emilian, R AU - Tonarini, S AU - Mason, P TI - Generation of normal and adakite-like calc-alkaline magmas in a non-subductional environment: An Sr-O-H isotopic study of the Apuseni Mountains neogene magmatic province, Romania JF - CHEMICAL GEOLOGY J2 - CHEM GEOL VL - 245 PY - 2007 IS - 1-2 SP - 70 EP - 88 PG - 19 SN - 0009-2541 DO - 10.1016/j.chemgeo.2007.07.027 UR - https://m2.mtmt.hu/api/publication/24849130 ID - 24849130 N1 - Cited By :27 Export Date: 15 June 2021 Correspondence Address: Seghedi, I.; Institute of Geodynamics, 19-21, Jean-Luis Calderon str., Bucharest 70201, Romania; email: seghedi@geodin.ro Funding details: 16258-N06 Funding details: Netherlands Research Centre for Integrated Solid Earth Sciences, ISES Funding text 1: We thank the Institute of Geodynamics (Bucharest) and Birkbeck University of London for support. Financial support has been obtained from Fonds für Wissenschaft und Forschung Projekt 16258-N06 and an ISES grant to I.S. for work in Utrecht in 2004. Z.D. Sharp and V. Atudorei (University of New Mexico) are kindly acknowledged for assistance during hydrogen isotope measurements and many interesting discussions. We thank the anonymous reviewers for their constructive reviews and Roberta Rudnick for her advice. LA - English DB - MTMT ER - TY - JOUR AU - Kovács, Sándor AU - Rálisch-Felgenhauer, E AU - Bóna, J TI - Conodont colour alteration related to a half-graben structure: an example from the Mesozoic of the Mecsek and Villány Hills area (Tisza Megaunit, Southern Hungary) JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 57 PY - 2006 IS - 4 SP - 257 EP - 268 PG - 12 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/152226 ID - 152226 N1 - Cited By :7 Export Date: 31 August 2023 Correspondence Address: Kovács, S.; Geological Research Group, Pazmany Peter setany 1/c, H-1117 Budapest, Hungary; email: skovacs@iris.geobio.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Barabás, A AU - Barabás-Stuhl, Á TI - Geology of the Lower Triassic Jakabhegy Sandstone Formation, Hungary, SE Transdanubia. JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 48 PY - 2005 IS - 1 SP - 1 EP - 47 PG - 47 SN - 0236-5278 DO - 10.1556/ageol.48.2005.1.1 UR - https://m2.mtmt.hu/api/publication/21491493 ID - 21491493 N1 - Cited By :8 Export Date: 15 June 2021 Correspondence Address: Barabás, A.Hajnóczy József u. 1, H-7633 Pécs, Hungary LA - English DB - MTMT ER - TY - BOOK AU - Császár, Géza TI - Magyarország és környezetének regionális földtana 1.. Paleozoikum-paleogén TS - Paleozoikum-paleogén ET - 0 PB - ELTE Eötvös Kiadó CY - Budapest PY - 2005 SP - 328 SN - 9634637442 UR - https://m2.mtmt.hu/api/publication/1449021 ID - 1449021 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Kovács, Sándor AU - Rálisch-Felgenhauer, E TI - Middle Anisian (Pelsonian) platform conodonts from the Triassic of the Mecsek Mts (South Hungary) - Their taxonomy and stratigraphic significance JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 48 PY - 2005 IS - 1 SP - 69 EP - 105 PG - 37 SN - 0236-5278 DO - 10.1556/AGeol.48.2005.1.3 UR - https://m2.mtmt.hu/api/publication/27161018 ID - 27161018 N1 - Cited By :14 Export Date: 15 June 2021 Correspondence Address: Kovács, S.; Geological Research Group, Pazmany P. setany 1/c, H-1117 Budapest, Hungary; email: skovacs@iris.geobio.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Kovács, Sándor AU - Bóna, J AU - Rálisch-Felgenhauer, E TI - Middle Anisian (Pelsonian) platform conodonts from the Triassic of the Villány Hills, South Hungary JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 48 PY - 2005 IS - 1 SP - 107 EP - 115 PG - 9 SN - 0236-5278 DO - 10.1556/AGeol.48.2005.1.4 UR - https://m2.mtmt.hu/api/publication/21491542 ID - 21491542 N1 - Cited By :7 Export Date: 15 June 2021 Correspondence Address: Kovács, S.; Geological Research Group, Pazmany P. setany 1/c, H-1117 Budapest, Hungary; email: skovacs@iris.geobio.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Csontos, L AU - Vörös, Attila TI - Mesozoic plate tectonic reconstruction of the carpathian region JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 210 PY - 2004 IS - 1 SP - 1 EP - 56 PG - 56 SN - 0031-0182 DO - 10.1016/j.palaeo.2004.02.033 UR - https://m2.mtmt.hu/api/publication/1236932 ID - 1236932 N1 - Cited By :483 Export Date: 11 November 2022 CODEN: PPPYA Correspondence Address: Csontos, L.; Geological Department, Pazmany P: setany 1/a, Budapest 1117, Hungary; email: csontos@ludens.elte.hu Funding details: Hungarian Science Foundation, T 037595, T 043760 Funding text 1: The authors are indebted to many colleagues for the discussions of earlier oral and written versions of the manuscript. We would like to thank especially F. Horváth, A. Galácz, S. Kovács, M. Kázmér, E. Márton (Budapest), D. Plašienka, M. Kováč (Bratislava), F. Neubauer and Č. Tomek (Salzburg), K. Birkenmajer (Kraków), M. Săndulescu (Bucharest) S. Schmid (Basel) and P. Ziegler (Basel). We express our thanks to W. Frisch, F. Horváth, G. Stampfli, Alonso-Gutierrez, J. Von Raumer, B. Murphy, A. Collins and D. Nance who kindly revised and improved earlier versions of the manuscript. This version was helped by critical remarks of K. Birkenmajer, F. Neubauer, B. Sperner, G. Stampfli, and F. Surlyk. IGCP project 453 is gratefully thanked for moral and material support. Hungarian Science Foundation OTKA projects T 043760, T 037595 are also thanked for support. AB - Palaeomagnetic, palaeobiogeographic and structural comparisons of different parts of the Alpine-Carpathian region suggest that four terranes comprise this area: the Alcapa, Tisza, Dacia and Adria terranes. These terranes are composed of different Mesozoic continental and oceanic fragments that were each assembled during a complex Late Jurassic-Cretaceous Palaeogene history. Palaeomagnetic and tectonic data suggest that the Carpathians are built up by two major oroclinal bends. The Alcapa bend has the Meliata oceanic unit, correlated with the Dinaric Vardar ophiolite, in its core. It is composed of the Western Carpathians, Eastern Alps and Southern Alcapa units (Transdanubian Range, Bukk). This terrane finds its continuation in the High Karst margin of the Dinarides. Further elements of the Alcapa terrane are thought to be derived from collided microcontinents: Czorsztyn in the N and a carbonate unit (Tisza?) in the SE. The Tisza-Dacia bend has the Vardar oceanic unit in its core. It is composed of the Bihor and Getic microcontinents. This terrane finds its continuation in the Serbo-Macedonian Massif of the Balkans. The Bihor-Getic microcontinent originally laid east of the Western Carpathians and filled the present Carpathian embayment in the Late Palaeozoic-Early Mesozoic. The Vardar ocean occupied an intermediate position between the Western Carpathian-Austroalpine-Transdanubian-High Karst margin and the Bihor-Getic-Serbo-Macedonian microcontinent. The Vardar and Pindos oceans were opened in the heart of the Mediterranean-Adriatic microcontinent in the Late Permian-Middle Triassic. Vardar subducted by the end of Jurassic, causing the Bihor-Getic-Serbo-Macedonian microcontinent to collide with the internal Dinaric-Western Carpathian margin. An external Penninic-Vahic ocean tract began opening in the Early Jurassic, separating the Austroalpine-Western Carpathian microcontinent (and its fauna) from the European shelf. Further east, the Severin-Ceahlau-Magura also began opening in the Early Jurassic, but final separation of the Bihor-Getic ribbon (and its fauna) from the European shelf did not take place until the late Middle Jurassic. The Alcapa and the Tisza-Dacia were bending during the Albian-Maastrichtian. The two oroclinal bends were finally opposed and pushed into the gates of the Carpathian embayment during the Palaeogene and Neogene. At that time, the main NS shortening in distant Alpine and Hellenic sectors was linked by a broader right-lateral shear zone along the former Vardar suture. (C) 2004 Elsevier B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Péró, Csaba TI - Mesozoic evolution of the Tisza Mega-unit JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 93 PY - 2004 IS - 2 SP - 297 EP - 313 PG - 17 SN - 1437-3254 DO - 10.1007/s00531-004-0384-9 UR - https://m2.mtmt.hu/api/publication/1019054 ID - 1019054 N1 - Cited By :137 Export Date: 11 November 2022 CODEN: IJESF Correspondence Address: Haas, J.; Geological Research Group, , Budapest 1117, Hungary; email: haas@ludens.elte.hu Funding details: Hungarian Scientific Research Fund, OTKA, T037595 Funding details: Magyar Tudományos Akadémia, MTA Funding text 1: Acknowledgement This study was supported by the Hungarian Academy of Sciences and the Hungarian Scientific Research Fund (OTKA Project T037595) The authors thank Professor Stefan Schmid and S ndor Kov cs for helpful discussions and comments. We are much obliged to Professor Wolfgang Frisch and Professor Peter Faupl for their careful and constructive reviews. Authors are indebted to Henry Lieberman (Houston, USA) for the lingual corrections. LA - English DB - MTMT ER - TY - JOUR AU - Harangi, Szabolcs AU - Tonarini, S AU - Vaselli, O AU - Manetti, P TI - Geochemistry and petrogenesis of Early Cretaceous alkaline igneous rocks in Central Europe: implications for a long-lived EAR-type mantle component beneath Europe. JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 46 PY - 2003 IS - 41 SP - 77 EP - 94 PG - 18 SN - 0236-5278 DO - 10.1556/AGeol.46.2003.1.6 UR - https://m2.mtmt.hu/api/publication/1855086 ID - 1855086 N1 - Department of Petrology/Geochemistry, Eotvös Loránd Univ., Pazmany Peter setány 1/C, Budapest H-1117, Hungary CNR-Inst. of Geosciences/Earth Rsrc., Viale Moruzzi 1, Pisa 56124, Italy Department of Earth Sciences, University of Florence, Via G. La Pira, 4, Florence 50121, Italy Cited By :23 Export Date: 13 January 2023 Correspondence Address: Harangi, S.; Department of Petrology/Geochemistry, Pazmany Peter setány 1/C, Budapest H-1117, Hungary; email: szabolcs.harangi@geology.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Csontos, L AU - Márton, E AU - Wórum, G AU - Benkovics, L TI - Geodynamics of SW-Pannonian inselbergs (Mecsek and Villány Mts, SW Hungary): Inferences from a complex structural analysis JF - EGU STEPHAN MUELLER SPECIAL PUBLICATION SERIES J2 - EGU STEPHAN MUELLER SPEC PUBL SER VL - 3 PY - 2002 SP - 227 EP - 245 PG - 19 SN - 1868-4556 UR - https://m2.mtmt.hu/api/publication/22242043 ID - 22242043 LA - English DB - MTMT ER - TY - JOUR AU - Csontos, László AU - Benkovics, L AU - Bergerat, F AU - Mansy, JL AU - Worum, G TI - Tertiary deformation history from seismic section study and fault analysis in a former European Tethyan margin (the Mecsek-Villany area, SW Hungary) JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 357 PY - 2002 IS - 1-4 SP - 81 EP - 102 PG - 22 SN - 0040-1951 DO - 10.1016/S0040-1951(02)00363-3 UR - https://m2.mtmt.hu/api/publication/2899890 ID - 2899890 N1 - Cited By :51 Export Date: 20 January 2023 Correspondence Address: Csontos, L.; Geological Department, Pazmany Péter setany l/c, Budapest 1117, Hungary; email: hungary.laszlo.csontos@ludens.elte.hu AB - Outcrop-scale structural data and seismic section interpretation are combined to unveil a very complicated Tertiary deformation history of a once Tethyan margin: the Mecsek-Villany area of Hungary. This combination of data helped to reconstruct the possible activity of individual fault zones. At least four ENE-WSW striking zones-the Northern Imbricates, the South Mecsek zone, the Gorcsony-Mariakemend ridge and the Villany Mountains-were confirmed as regional long-lived transpressive zones with very complicated internal deformation, frequently with oppositely dipping thrust faults. Tertiary structural history began with a roughly N-S-directed shortening in the South Mecsek zone. It was followed by a NE-SW-directed transpression activating practically all important wrench zones together with perpendicular transfer faults. Basins were created along some of these deformation zones, but were also affected by major tilts due to inversion. After a relatively quiescent period in the Middle Miocene, the Late Sarmatian inversion followed. Shortly after, this event was relayed by a NE-SW-directed extension-transtension. An important inversion period characterised by NW-SE compression occurred in Late Pannonian (Messinian), when all the former wrench zones were reactivated as right-lateral shear. This event is responsible for the present topography of the region. (C) 2002 Elsevier Science B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Hips, Kinga AU - Pelikán, P TI - Lower Triassic shallow marine succession in the Bükk Mountains, NE Hungary JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 53 PY - 2002 IS - 6 SP - 351 EP - 367 PG - 17 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/152249 ID - 152249 LA - English DB - MTMT ER - TY - JOUR AU - Onac, B P TI - Caves formed within Upper Cretaceous skarns at Bǎiţa Bihor County, Romania: Mineral deposition and speleogenesis JF - CANADIAN MINERALOGIST J2 - CAN MINERAL VL - 40 PY - 2002 IS - 6 SP - 1693 EP - 1703 PG - 11 SN - 0008-4476 DO - 10.2113/gscanmin.40.6.1693 UR - https://m2.mtmt.hu/api/publication/21491550 ID - 21491550 N1 - Cited By :12 Export Date: 15 June 2021 CODEN: CAMIA Correspondence Address: Onac, B.P.; Department of Mineralogy, , Cluj 3400, Romania; email: bonac@bioge.ubbcluj.ro LA - English DB - MTMT ER - TY - JOUR AU - Neugebauer, J AU - Greiner, B AU - Appel, E TI - Kinematics of the Alpine-West Carpathian orogen and palaeogeographic implications JF - JOURNAL OF THE GEOLOGICAL SOCIETY J2 - J GEOL SOC LONDON VL - 158 PY - 2001 IS - Part 1 SP - 97 EP - 110 PG - 14 SN - 0016-7649 DO - 10.1144/jgs.158.1.97 UR - https://m2.mtmt.hu/api/publication/20045897 ID - 20045897 N1 - Cited By :61 Export Date: 8 September 2023 Correspondence Address: Neugebauer, J.; Institute Geology and Palaeontology, , Tuebingen D-72116, Germany; email: joachim.neugebauer@uni-tuebingen.de LA - English DB - MTMT ER - TY - JOUR AU - Árkai, Péter AU - Bérczi, Makk A AU - Balogh, Kadosa TI - Alpine low-T prograde metamorphism in the post-Variscan basement of the Great Plain, Tisza Unit (Pannonian Basin, Hungary) JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 43 PY - 2000 IS - 1 SP - 43 EP - 63 PG - 21 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1098540 ID - 1098540 LA - English DB - MTMT ER - TY - JOUR AU - Kovács, Sándor AU - Szederkényi, T AU - Haas, János AU - Buda, György AU - Császár, Géza AU - Nagymarosy, András TI - Tectonostratigraphic terranes in the pre-Neogene basement of the Hungarian part of the Pannonian area JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 43 PY - 2000 IS - 3 SP - 225 EP - 328 PG - 104 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/152233 ID - 152233 N1 - Cited By :96 Export Date: 13 January 2023 Correspondence Address: Kovávs, S.; Geological Research Group, Muzeum krt. 4/a, Budapest, Buda H-1088, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Török, Ákos TI - Formation of dolomite mottling in Middle Triassic ramp carbonates (Southern Hungary) JF - SEDIMENTARY GEOLOGY J2 - SEDIMENT GEOL VL - 131 PY - 2000 IS - 3-4 SP - 131 EP - 145 PG - 15 SN - 0037-0738 DO - 10.1016/S0037-0738(99)00137-2 UR - https://m2.mtmt.hu/api/publication/1635943 ID - 1635943 N1 - Cited By :17 Export Date: 15 June 2021 Correspondence Address: Torok, A.; Department of Engineering Geology, , H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu Funding details: Hungarian Scientific Research Fund, OTKA, F026401 Funding details: Országos Muszaki Fejlesztési Bizottság, OMFB Funding text 1: P. Frykman, E. Nygaard, C.K. Claussen (Geological Survey of Denmark), B. Sellwood, V.P. Wright (Postgraduate Research Institute for Sedimentology, Reading University) provided much help during my stays in Denmark and the UK and ensured technical facilities. The enormous work of C. Braithwaite and P. Muchez in correcting the manuscript, their useful comments and suggestions are very much appreciated. The critical review of H. Qing has also improved the quality of the paper. I am grateful to A. Demény and A. Mindszenty for consultations. Technical help of E. Horthy, Cs. Péró and E. Sasköi is appreciated. A mobility grant was given by the Széchenyi Foundation to the University of Reading. Financial support was partly provided by Hungarian Scientific Research Foundation (OTKA, F026401) and by OMFB. LA - English DB - MTMT ER - TY - JOUR AU - Vörös, Attila TI - The Triassic of the Alps and Carpathians and its interregional correlation JF - DEVELOPMENTS IN PALAEONTOLOGY AND STRATIGRAPHY J2 - DEVEL PALAEONT STRATIGR VL - 18 PY - 2000 IS - C SP - 173 EP - 196 PG - 24 SN - 0920-5446 DO - 10.1016/S0920-5446(00)80011-4 UR - https://m2.mtmt.hu/api/publication/22874257 ID - 22874257 AB - The Triassic stratigraphy and facies of the four major terranes of the Alpine-Carpathian region is shortly described and illustrated by schematic stratigraphic charts. The main stratigraphical features of the terranes are compared to those of the neighbouring epicontinental regions (Europe and North Africa) and the Aegean region, representing the Tethyan domain. The detailed ammonoid biostratigraphical subdivision developed in the Alpine region is also correlated with the neighbouring regions. The paleogeographical positions of the terranes are briefly discussed. It is concluded that the crustal fragments carrying the later Alpine-Carpathian terranes were in close connection with the Eurasian continental shelf in the Triassic, while during the Jurassic they belonged to different microcontinents within the western Tethys ocean. © 2000 Elsevier B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Tari, Gábor AU - Dövényi, Péter AU - Dunkl, István AU - Horváth, Ferenc AU - Lenkey, László AU - Szafian, P AU - Toth, T TI - Lithospheric structure of the Pannonian basin derived from seismic, gravity and geothermal data JF - GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS J2 - GEOL SOC SPEC PUBL VL - 156 PY - 1999 SP - 215 EP - 250 PG - 36 SN - 0305-8719 DO - 10.1144/GSL.SP.1999.156.01.12 UR - https://m2.mtmt.hu/api/publication/1256307 ID - 1256307 AB - This paper is part of the special publication No.156, The Mediterranean basins: Tertiary extension within the Alpine Orogen. (eds B.Durand, L. Jolivet, F.Horvath and M.Seranne). The structure of the Pannonian basin is the result of distinct modes of Mid-Late Miocene extension exerting a profound effect on the lithospheric configuration, which continues even today. As the first manifestation of extensional collapse, large magnitude, metamorphic core complex style extension took place at the beginning of the Mid-Miocene in certain parts of the basin. Extrapolation of the present-day high heat flow in the basin, corrected for the blanketing effect of the basin fill, indicates a hot and thin lithosphere at the onset of extension. This initial condition, combined with the relatively thick crust inherited from earlier Alpine compressional episodes, appears to be responsible for the core complex type extension at the beginning of the syn-rift period. This type of extension is well documented in the northwestern Pannonian basin. Newly obtained deep reflection seismic and fission-track data integrated with well data from the southeastern part of the basin suggests that it developed in a similar fashion. Shortly after the initial period, the style of syn-rift extension changed to a wide-rift style, covering an area of much larger geographic extent. The associated normal faults revealed by industry reflection seismic data tend to dominate within the upper crust, obscuring pre-existing structures. However, several deep seismic profiles, constrained by gravity and geothermal modeling, image the entire lithosphere beneath the basin. It is the Mid-Miocene synrift extension which is still reflected in the structure of the Pannonian lithosphere, on the scale of the whole basin system. The gradually diminishing extension during the Late Miocene/Pliocene could not advance to the localization of extension into narrow rift zones in the Pannonian region except some deep subbasins such as the Mako/Bekes and Danube basins. These basins are underlain coincidently by anomalously thin crust (22-25 km) and lithosphere (45-60 km). Significant departures (up to 130 mW m -2) from the average present-day surface heat flow for the initiation of two newly defined narrow rift zones (Tisza and Duna) in the Pannonian basin system. However, both of these narrow rifts failed since the final docking of the Eastern Carpathians onto the European foreland excluded any further extension of the back-arc region. LA - English DB - MTMT ER - TY - JOUR AU - Török, Ákos TI - Petrophysical and sedimentological analyses of Siklós ornamental limestones, S-Hungary JF - PERIODICA POLYTECHNICA-CIVIL ENGINEERING J2 - PERIOD POLYTECH CIV ENG VL - 43 PY - 1999 IS - 2 SP - 187 EP - 205 PG - 19 SN - 0553-6626 UR - https://m2.mtmt.hu/api/publication/1635953 ID - 1635953 N1 - Cited By :3 Export Date: 15 June 2021 CODEN: PPCBA Correspondence Address: Torok, A.; Department of Engineering Geology, , H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu Cited By :3 Export Date: 18 June 2021 CODEN: PPCBA Correspondence Address: Torok, A.; Department of Engineering Geology, , H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu Cited By :3 Export Date: 1 September 2021 CODEN: PPCBA Correspondence Address: Torok, A.; Department of Engineering Geology, , H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu Cited By :3 Export Date: 3 September 2021 CODEN: PPCBA Correspondence Address: Torok, A.; Department of Engineering Geology, , H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu LA - English DB - MTMT ER - TY - JOUR AU - Fodor, László AU - Csontos, László TI - Magyarországi szerkezetföldtani kutatások és ezek legújabb eredményei JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 128 PY - 1998 IS - 1 SP - 123 EP - 143 PG - 21 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1368457 ID - 1368457 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Hips, Kinga TI - Lower Triassic storm-dominated ramp sequence in northern Hungary: An example of evolution from homoclinal through distally steepened ramp to Middle Triassic flat-topped platform. JF - GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS J2 - GEOL SOC SPEC PUBL VL - 149 PY - 1998 SP - 315 EP - 338 PG - 24 SN - 0305-8719 DO - 10.1144/GSL.SP.1999.149.01.15 UR - https://m2.mtmt.hu/api/publication/21491561 ID - 21491561 LA - English DB - MTMT ER - TY - JOUR AU - Konrád, Gyula TI - Synsedimentary tectonic events in the Middle Triassic evolution of the SE Transdanubian part of the Tisza Unit JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 41 PY - 1998 IS - 3 SP - 327 EP - 341 PG - 15 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1324065 ID - 1324065 LA - English DB - MTMT ER - TY - JOUR AU - Pamic, J AU - Gusic, I AU - Jelaska, V TI - Geodynamic evolution of the central Dinarides. JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 297 PY - 1998 IS - 1-4 SP - 251 EP - 268 PG - 18 SN - 0040-1951 DO - 10.1016/S0040-1951(98)00171-1 UR - https://m2.mtmt.hu/api/publication/21491562 ID - 21491562 N1 - Croatian Acad. of Sciences and Arts, Ante Kovačića 5, 10000 Zagreb, Croatia Department of Geology, Faculty of Science, University of Zagreb, Zvonimirova 8, 10000 Zagreb, Croatia Cited By :192 Export Date: 15 June 2021 Correspondence Address: Pamic, J.; Croatian Academy of Sci. and Arts, Ante Kovacica 5, 10000 Zagreb, Croatia LA - English DB - MTMT ER - TY - JOUR AU - Török, Ákos TI - Controls on development of Mid-Triassic ramps: examples from southern Hungary JF - GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS J2 - GEOL SOC SPEC PUBL VL - 149 PY - 1998 SP - 339 EP - 367 PG - 29 SN - 0305-8719 DO - 10.1144/GSL.SP.1999.149.01.16 UR - https://m2.mtmt.hu/api/publication/1635999 ID - 1635999 N1 - Cited By :41 Export Date: 15 June 2021 Correspondence Address: Török, Á.; Department of Geology, Sztoczek u. 2, H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu AB - During Mid-Triassic time the palaeogeographical-tectonic setting of the northern Tethyan passive margin and epicontinental basins favoured the ramp morphology, as broad flat areas were available for flooding and establishment of carbonate sedimentation. Throughout this time, in what is now southern Hungary, homoclinal ramps developed, which also exhibit some evidence of partial distal steepening. The nearly 1 km thick Anisian-Ladinian Muschelkalk carbonates are grouped into six depositional units. In each ramp unit facies types were identified representing coastal sabkhas, inner ramp peritidal facies, backshoal lagoons, oolite shoals, storm to fair-weather influenced mid-ramps, proximal to distal shell beds and low-energy outer ramps. Mid- and inner ramp carbonates make up the majority of the successions. The deepest outer ramp facies correspond to the peak transgression of a second-order Triassic sea-level rise. In the Hungarian Muschelkalk three major transgressive-regressive sequences were identified. In Germany, Poland and Spain much thinner and slightly coarser Muschelkalk carbonate successions were formed in the same Mid-Triassic interval. The major sediment redistribution processes were related to storms that generated coquinas, and mud flow deposits. Slow, early diagenesis and the predominance of unstable muddy substrate led to the formation of small-scale slumps, slides and plastic deformation. The fauna reflects the prevalence of carbonate mud and temporarily high-stress conditions. A non 'cool water' origin of this ramp is inferred from the presence of evaporites, early dolomization of inner ramp carbonates, the biota and the palaeogeographical setting. The major controlling factors of Mid-Triassic ramps were the gentle antecedent morphology, the subtropical climate, the high production of carbonate mud and the lack of reef-building organisms, as well as the passive margin setting, which resulted in a moderate and relatively uniform subsidence rate over a wide area. LA - English DB - MTMT ER - TY - JOUR AU - Szente, István TI - Bivalve assemblages from the Middle Triassic Muschelkalk of the Mecsek Mts, South Hungary: An overview JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 40 PY - 1997 IS - 4 SP - 411 EP - 424 PG - 14 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/2224128 ID - 2224128 N1 - Department of Palaeontology, Eötvös University, Budapest, Hungary Ludovika tér 2, H-1083 Budapest, Hungary Cited By :13 Export Date: 25 March 2024 Correspondence Address: Szente, I.Ludovika tér 2, H-1083 Budapest, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Török, Ákos TI - Dolomitization and karst-related dedolomitzation of Muschelkalk carbonates, in South Hungary JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 40 PY - 1997 IS - 4 SP - 441 EP - 462 PG - 22 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1635954 ID - 1635954 N1 - Budapest Technical University, Department of Engineering Geology, Hungary Sztoczek u. 2, H-1521 Budapest, Hungary Cited By :6 Export Date: 15 June 2021 Correspondence Address: Török, Á.Sztoczek u. 2, H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu Budapest Technical University, Department of Engineering Geology, Hungary Sztoczek u. 2, H-1521 Budapest, Hungary Cited By :6 Export Date: 18 June 2021 Correspondence Address: Török, Á.Sztoczek u. 2, H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu LA - English DB - MTMT ER - TY - JOUR AU - Török, Ákos TI - Triassic ramp evolution, southern Hungary and its similarities to Germano-type Triassic. JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 40 PY - 1997 IS - 4 SP - 367 EP - 390 PG - 24 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1635955 ID - 1635955 N1 - Budapest Technical University, Department of Engineering Geology, Hungary Sztoczek u. 2, H-1521 Budapest, Hungary Cited By :15 Export Date: 15 June 2021 Correspondence Address: Török, Á.Sztoczek u. 2, H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu Budapest Technical University, Department of Engineering Geology, Hungary Sztoczek u. 2, H-1521 Budapest, Hungary Cited By :15 Export Date: 16 June 2021 Correspondence Address: Török, Á.Sztoczek u. 2, H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu Budapest Technical University, Department of Engineering Geology, Hungary Sztoczek u. 2, H-1521 Budapest, Hungary Cited By :15 Export Date: 30 August 2021 Correspondence Address: Török, Á.Sztoczek u. 2, H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu LA - English DB - MTMT ER - TY - JOUR AU - Harangi, Szabolcs AU - Szabó, Csaba AU - Józsa, Sándor AU - Szoldán, Z AU - Árva-Sós, Erzsébet AU - Balla, Márta AU - Kubovics, Imre TI - Mesozoic igneous suites in Hungary: Implications for genesis and tectonic setting in the northwestern part of Tethys JF - INTERNATIONAL GEOLOGY REVIEW J2 - INT GEOL REV VL - 38 PY - 1996 IS - 4 SP - 336 EP - 360 PG - 25 SN - 0020-6814 DO - 10.1080/00206819709465339 UR - https://m2.mtmt.hu/api/publication/1412630 ID - 1412630 N1 - Department of Petrology and Geochemistry, Eötvös University, Múzeum krt. 4/A, Budapest, 1088, Hungary Department of Isotope Analysis, Institute of Nuclear Research, Hungarian Academy of Sciences, Debrecen, Bern tér, 18c 4001, Hungary Institute of Nuclear Technology, Technical University, Budapest, 1521, Hungary Department of Petrology and Geochemistry, Eötvös University, Múzeum krt. 4/A, Budapest, 1088, Hungary Cited By :66 Export Date: 17 January 2023 AB - Mesozoic igneous rocks occur in various tectonic units of the Intra-Carpathian Area of Eastern Europe. These rocks were situated several hundred km apart from one another during their formation, and subsequent large lateral displacements resulted in their present positions. They formed during a relatively wide temporal range (Middle Triassic to Late Cretaceous) through different petrogenetic processes associated with the Mesozoic evolution of the northwestern part of Tethys. In the Transdanubian subunit of the Alcapa block, Middle Triassic calc-alkaline, intermediateto-acidic, and potassic rocks occur as pyroclastics, lava flows, and dikes in the Bakony and Buda mountains. The Gemer-Bükk subunit of the Alcapa block comprises two different igneous series: (1) slightly metamorphosed Middle Triassic volcanic rocks of the Eastern Bükk Mountains, which can be divided into an older (Anisian-Early Ladinian) calc-alkaline, intermediateto-acidic volcanic series and a younger (Late Ladinian) alkaline basaltic series; and (2) two series of the Middle Triassic to Middle Jurassic ophiolite complex (Bódva Magmatic Series and Darnó-Szarvaskö Magmatic Series), embedded in a tectonic mélange and in an olistostrome suite along a SW-NE-oriented zone. The Tisza block contains Early Cretaceous alkaline volcanic rocks in the Mecsek-Alföld subunit. Strong temporal and geochemical correlations have been observed between the Middle Triassic volcanic rocks of the Bakony and Buda mountains and the Southern Alps, and those of the Eastern Bükk Mountains and the Outer Dinarides. We propose that all these rocks were formed during the same extension-related volcanic activity along the Southern Alps-Bakony and Buda mountains-Eastern Bükk Mountains-Dinarides region. The Middle Triassic-Middle Jurassic ultramafic-mafic igneous rocks of the Gemer-Bükk subunit can be correlated with the ophiolites of the Inner Dinarides. Geochemistry of the mafic rocks is consistent with an origin from an N-MORB and E-MORB source mantle. The Middle to Late Triassic ultramafic and mafic rocks of the Bódva and Darnó-Szarvaskö series could have originated along the mid-oceanic ridge system of the northwestern segment of the Vardar ocean (Meliaticum). The Middle Jurassic igneous rocks of the Darnó-Szarvaskö series could have corresponded to the opening of a backarc basin. Early Cretaceous alkaline volcanic rocks of the Mecsek-Alföld zone in the Tisza block formed as a result of continental rifting along the southern margin of the European plate. Two volcanic series - a mafic and a sodic group - were generated from an OIB-like asthenospheric mantle. Separation of the Tisza block from the European plate occurred contemporaneously with volcanic activity during the late Early Cretaceous. LA - English DB - MTMT ER - TY - JOUR AU - Hips, Kinga TI - Stratigraphical and facies evaluation of the Lower Triassic formations in the Aggtelek-Rudabánya Mountains, NE Hungary JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 39 PY - 1996 IS - 4 SP - 369 EP - 411 PG - 43 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/152253 ID - 152253 N1 - Academical Research Group, Department of Geology, Eötvös Univ. of Sciences, Budapest, Hungary Múzeum krt. 4/A, H-1088 Budapest, Hungary Cited By :20 Export Date: 2 June 2023 Correspondence Address: Hips, K.Múzeum krt. 4/A, H-1088 Budapest, Hungary LA - English DB - MTMT ER -