@article{MTMT:3385746, title = {„Oázis a sivatagban” — különösen gazdag ősmaradvány-együttes a fosszíliaszegény üllési Szegedi Dolomitból}, url = {https://m2.mtmt.hu/api/publication/3385746}, author = {Szurominé, Korecz Andrea and Garaguly, István and Szente, István and Raucsikné Varga, Andrea Beáta and Raucsik, Béla}, doi = {10.23928/foldt.kozl.2018.148.2.119}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {148}, unique-id = {3385746}, issn = {0015-542X}, year = {2018}, eissn = {2559-902X}, pages = {119-124}, orcid-numbers = {Garaguly, István/0000-0002-2802-0738; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974} } @article{MTMT:3202162, title = {Középső-triász dolomitok képződésének története és töréses deformációja a Szegedi-medence területén}, url = {https://m2.mtmt.hu/api/publication/3202162}, author = {Garaguly, István and Raucsik, Béla and Raucsikné Varga, Andrea Beáta and Schubert, Félix}, doi = {10.23928/foldt.kozl.2017.147.1.39}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {147}, unique-id = {3202162}, issn = {0015-542X}, year = {2017}, eissn = {2559-902X}, pages = {39-60}, orcid-numbers = {Garaguly, István/0000-0002-2802-0738; Raucsik, Béla/0000-0002-1951-5974; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Schubert, Félix/0000-0001-8647-5354} } @article{MTMT:3091740, title = {Processes and controlling factors of polygenetic dolomite formation in the Transdanubian Range, Hungary: a synopsis}, url = {https://m2.mtmt.hu/api/publication/3091740}, author = {Haas, János and Hips, Kinga and Budai, Tamás and Győri, Orsolya and Lukoczki, Georgina and Kele, Sándor and Demény, Attila and Poros, Zsófia}, doi = {10.1007/s00531-016-1347-7}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {106}, unique-id = {3091740}, issn = {1437-3254}, year = {2017}, eissn = {1437-3262}, pages = {991-1021}, orcid-numbers = {Haas, János/0000-0003-0929-8889; Hips, Kinga/0000-0003-2315-120X; Győri, Orsolya/0000-0002-3646-9113; Lukoczki, Georgina/0000-0002-0661-0198; Kele, Sándor/0000-0002-8607-7636; Demény, Attila/0000-0003-0522-9018} } @article{MTMT:3304112, title = {A dorozsmai márvány (Tiszai-főegység) kőzettani újravizsgálata: deformáció és fluidum hatása a mikroszerkezet fejlődésére}, url = {https://m2.mtmt.hu/api/publication/3304112}, author = {Papp, Nikoletta and Raucsikné Varga, Andrea Beáta and Mészáros, Előd and Raucsik, Béla}, doi = {10.23928/foldt.kozl.2017.147.4.337}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {147}, unique-id = {3304112}, issn = {0015-542X}, year = {2017}, eissn = {2559-902X}, pages = {337-356}, orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Mészáros, Előd/0000-0002-5846-9034; Raucsik, Béla/0000-0002-1951-5974} } @article{MTMT:3042991, title = {Recrystallization-induced oxygen isotope changes in inclusion-hosted water of speleothems - Paleoclimatological implications}, url = {https://m2.mtmt.hu/api/publication/3042991}, author = {Demény, Attila and Czuppon, György and Kern, Zoltán and Leél-Őssy, Szabolcs and Németh, Alexandra and Szabó, Máté Zoltán and Tóth, Mária and Wu, C-C and Shen, C-C and Molnár, Mihály and Németh, Tibor and Németh, Péter and Óvári, Mihály}, doi = {10.1016/j.quaint.2015.11.137}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {415}, unique-id = {3042991}, issn = {1040-6182}, abstract = {The issue of diagenetic alteration of carbonate deposits in caves (speleothems) has gained increasing importance in recent years, as this process has serious consequences for speleothem-based paleoclimate studies. In this study stable hydrogen and oxygen isotope data of water trapped in fluid inclusions were collected for recently forming stalagmites and flowstones in order to determine how dripwater compositions are reflected and preserved in the inclusion water compositions. Hydrogen isotope compositions were found to reflect dripwater values, whereas the oxygen isotope data were increasingly shifted from the local dripwater compositions with the time elapsed after deposition. The δ18O data are correlated with X-Ray diffraction full width at half maximum values (related to crystal domain size and lattice strain), suggesting that the oxygen isotope shift is related to recrystallization of calcite. Transmission electron microscope analyses detected the presence of nanocrystalline (<50 nm) calcite, whose crystallization to coarser-grained calcite crystals (>200 nm) may have induced re-equilibration between the carbonate and the trapped inclusion water. The Ostwald ripening process provides an explanation for unexpectedly low oxygen isotope compositions in the inclusion water. The detected diagenetic alteration and its isotopic effects should be taken into consideration during sampling strategies and data evaluation as speleothems containing nanocrystalline calcite during their deposition are prone to late-stage oxygen isotope water-carbonate re-equilibration, which may shift the oxygen isotope composition of the inclusion water to more depleted values while the hydrogen isotope composition remains intact. © 2016.}, keywords = {fluid inclusion; speleothem; diagenesis; Ostwald ripening; Hydrogen and oxygen isotope compositions}, year = {2016}, eissn = {1873-4553}, pages = {25-32}, orcid-numbers = {Demény, Attila/0000-0003-0522-9018; Czuppon, György/0000-0002-7231-6042; Kern, Zoltán/0000-0003-4900-2587; Németh, Tibor/0000-0002-1836-6006; Németh, Péter/0000-0001-5592-5877} } @article{MTMT:2938240, title = {Hydrothermal dolomitization of basinal deposits controlled by a synsedimentary fault system in Triassic extensional setting, Hungary}, url = {https://m2.mtmt.hu/api/publication/2938240}, author = {Hips, Kinga and Haas, János and Győri, Orsolya}, doi = {10.1007/s00531-015-1237-4}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {105}, unique-id = {2938240}, issn = {1437-3254}, year = {2016}, eissn = {1437-3262}, pages = {1215-1231}, orcid-numbers = {Hips, Kinga/0000-0003-2315-120X; Haas, János/0000-0003-0929-8889; Győri, Orsolya/0000-0002-3646-9113} } @article{MTMT:3126648, title = {Palaeofluid evolution in a fractured basalt hosted reservoir in the Üllés-Ruzsa-Bordány area, southern sector of the Pannonian Basin}, url = {https://m2.mtmt.hu/api/publication/3126648}, author = {Szabó, B and Schubert, Félix and M. Tóth, Tivadar and Steinbach, Gábor}, doi = {10.4154/gc.2016.25}, journal-iso = {GEOL CROAT}, journal = {GEOLOGIA CROATICA}, volume = {69}, unique-id = {3126648}, issn = {1330-030X}, year = {2016}, eissn = {1333-4875}, pages = {281-293}, orcid-numbers = {Schubert, Félix/0000-0001-8647-5354; M. Tóth, Tivadar/0000-0003-1012-1095; Steinbach, Gábor/0000-0001-7137-7030} } @article{MTMT:2891033, title = {Genesis of Upper Triassic peritidal dolomites in the Transdanubian Range, Hungary}, url = {https://m2.mtmt.hu/api/publication/2891033}, author = {Haas, János and Lukoczki, Georgina and Budai, Tamás and Demény, Attila}, doi = {10.1007/s10347-015-0435-7}, journal-iso = {FACIES}, journal = {FACIES}, volume = {61}, unique-id = {2891033}, issn = {0172-9179}, year = {2015}, eissn = {1612-4820}, orcid-numbers = {Haas, János/0000-0003-0929-8889; Lukoczki, Georgina/0000-0002-0661-0198; Demény, Attila/0000-0003-0522-9018} } @article{MTMT:2815153, title = {Dolomitization of Triassic microbial mat deposits (Hungary): Origin of microcrystalline dolomite}, url = {https://m2.mtmt.hu/api/publication/2815153}, author = {Hips, Kinga and Haas, János and Poros, Zsófia and Kele, Sándor and Budai, Tamás}, doi = {10.1016/j.sedgeo.2014.12.002}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {318}, unique-id = {2815153}, issn = {0037-0738}, keywords = {Fluid inclusions; Stable carbon and oxygen isotopes; Organogenic dolomite; Microbial microfabric}, year = {2015}, eissn = {1879-0968}, pages = {113-129}, orcid-numbers = {Hips, Kinga/0000-0003-2315-120X; Haas, János/0000-0003-0929-8889; Kele, Sándor/0000-0002-8607-7636} } @article{MTMT:2949635, title = {Structural controls on petroleum migration and entrapment within the faulted basement blocks of Szeghalom Dome (Pannonian Basin, SE Hungary)}, url = {https://m2.mtmt.hu/api/publication/2949635}, author = {Molnár, L and M. Tóth, Tivadar and Schubert, Félix}, doi = {10.4154/gc.2015.19}, journal-iso = {GEOL CROAT}, journal = {GEOLOGIA CROATICA}, volume = {68}, unique-id = {2949635}, issn = {1330-030X}, year = {2015}, eissn = {1333-4875}, pages = {247-259}, orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354} } @article{MTMT:2779728, title = {Stable (H, O, C) and noble-gas (He and Ar) isotopic compositions from calcite and fluorite in the Speewah Dome, Kimberley Region, Western Australia: implications for the conditions of crystallization and evidence for the influence of crustal-mantle fluid mixing}, url = {https://m2.mtmt.hu/api/publication/2779728}, author = {Czuppon, György and Ramsay, RR and Özgenc, I and Demény, Attila and Gwalani, LG and Rogers, K and Eves, A and Papp, László and Palcsu, László and Berkesi, Márta and Downes, PJ}, doi = {10.1007/s00710-014-0333-7}, journal-iso = {MINER PETROL}, journal = {MINERALOGY AND PETROLOGY}, volume = {108}, unique-id = {2779728}, issn = {0930-0708}, year = {2014}, eissn = {1438-1168}, pages = {759-775}, orcid-numbers = {Czuppon, György/0000-0002-7231-6042; Demény, Attila/0000-0003-0522-9018; Berkesi, Márta/0000-0003-4380-057X} } @misc{MTMT:2546226, title = {Magyarország pre-kainozoos földtani térképe. [Pre-Cenozoic geological map of Hungary]}, url = {https://m2.mtmt.hu/api/publication/2546226}, author = {Haas, J and Budai, Tamás and Csontos, L and Fodor, László and Konrád, Gy}, unique-id = {2546226}, year = {2010} } @misc{MTMT:1369156, title = {Magyarország pre-kainozoos földtani térképe 1:500000 (Pre-Cenozoic geological map of Hungary, 1:5000000)}, url = {https://m2.mtmt.hu/api/publication/1369156}, author = {Haas, János and Budai, Tamás and Csontos, L and Fodor, László and Konrád, Gyula}, unique-id = {1369156}, year = {2010}, orcid-numbers = {Haas, János/0000-0003-0929-8889} } @article{MTMT:1382753, title = {Paleofluid evolution of the fractured basalt hydrocarbon reservoir in the Üllés–Ruzsa–Bordány area, SE Hungary}, url = {https://m2.mtmt.hu/api/publication/1382753}, author = {Szabó, B and Schubert, Félix and M. Tóth, Tivadar}, doi = {10.1556/CEuGeol.52.2009.3-4.6}, journal-iso = {CENT EUR GEOL}, journal = {CENTRAL EUROPEAN GEOLOGY}, volume = {52}, unique-id = {1382753}, issn = {1788-2281}, year = {2009}, eissn = {1789-3348}, pages = {299-323}, orcid-numbers = {Schubert, Félix/0000-0001-8647-5354; M. Tóth, Tivadar/0000-0003-1012-1095} } @article{MTMT:32550094, title = {Triassic}, url = {https://m2.mtmt.hu/api/publication/32550094}, author = {Feist-Burkhardt, S and Götz, AE and Szulc, J and Borkhataria, R and Geluk, M and Haas, János and Hornung, J and Jordan, P and Kempf, O and Michalík, J and Nawrocki, J and Reinhardt, L and Ricken, W and Röhling, HG and Rüffer, T and Török, Ákos and Zühlke, R}, journal-iso = {CENTRAL EUROPE}, journal = {CENTRAL EUROPE}, volume = {2}, unique-id = {32550094}, issn = {1479-0963}, year = {2008}, eissn = {1745-8218}, pages = {749-821}, orcid-numbers = {Haas, János/0000-0003-0929-8889; Török, Ákos/0000-0002-5394-4510} } @article{MTMT:1129827, title = {Fluid-inclusion evidence of petroleum migration through a buried metamorphic dome in the Pannonian Basin, Hungary}, url = {https://m2.mtmt.hu/api/publication/1129827}, author = {Schubert, Félix and Diamond, L W and M. Tóth, Tivadar}, doi = {10.1016/j.chemgeo.2007.05.019}, journal-iso = {CHEM GEOL}, journal = {CHEMICAL GEOLOGY}, volume = {244}, unique-id = {1129827}, issn = {0009-2541}, year = {2007}, eissn = {1872-6836}, pages = {357-381}, orcid-numbers = {Schubert, Félix/0000-0001-8647-5354; M. Tóth, Tivadar/0000-0003-1012-1095} } @article{MTMT:1236932, title = {Mesozoic plate tectonic reconstruction of the carpathian region}, url = {https://m2.mtmt.hu/api/publication/1236932}, author = {Csontos, L and Vörös, Attila}, doi = {10.1016/j.palaeo.2004.02.033}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {210}, unique-id = {1236932}, issn = {0031-0182}, abstract = {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.}, year = {2004}, eissn = {1872-616X}, pages = {1-56} } @article{MTMT:1019054, title = {Mesozoic evolution of the Tisza Mega-unit}, url = {https://m2.mtmt.hu/api/publication/1019054}, author = {Haas, János and Péró, Csaba}, doi = {10.1007/s00531-004-0384-9}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {93}, unique-id = {1019054}, issn = {1437-3254}, year = {2004}, eissn = {1437-3262}, pages = {297-313}, orcid-numbers = {Haas, János/0000-0003-0929-8889} } @article{MTMT:1891351, title = {A pannóniai Tótkomlósi Mészmárga Tagozat kifejlődése és kora a Battonya-pusztaföldvári-hátság környezetében. The Tótkomlós Calcareous Marl Member of the Lake Pannon sedimentary sequence in the Battonya-Pusztaföldvár region, SE Hungary}, url = {https://m2.mtmt.hu/api/publication/1891351}, author = {Magyar, Imre and Juhász, Gy and Szuromi-Korecz, A and Sütő-Szentai, M}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {133}, unique-id = {1891351}, issn = {0015-542X}, year = {2004}, eissn = {2559-902X}, pages = {521-540} } @article{MTMT:1129807, title = {Connected fluid evolution in fractured crystalline basement and overlying sediments, Pannonian Basin, SE Hungary}, url = {https://m2.mtmt.hu/api/publication/1129807}, author = {Juhász, A and M. Tóth, Tivadar and Ramseyer, K and Matter, A}, doi = {10.1016/S0009-2541(01)00269-8}, journal-iso = {CHEM GEOL}, journal = {CHEMICAL GEOLOGY}, volume = {182}, unique-id = {1129807}, issn = {0009-2541}, year = {2002}, eissn = {1872-6836}, pages = {91-120}, orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095} } @inbook{MTMT:152295, title = {Geological setting and tectonic evolution of Hungary}, url = {https://m2.mtmt.hu/api/publication/152295}, author = {Haas, János and Hámor, G and Korpás, L}, booktitle = {Carlin gold in Hungary}, unique-id = {152295}, year = {1999}, pages = {179-196}, orcid-numbers = {Haas, János/0000-0003-0929-8889} } @article{MTMT:1256307, title = {Lithospheric structure of the Pannonian basin derived from seismic, gravity and geothermal data}, url = {https://m2.mtmt.hu/api/publication/1256307}, author = {Tari, Gábor and Dövényi, Péter and Dunkl, István and Horváth, Ferenc and Lenkey, László and Szafian, P and Toth, T}, doi = {10.1144/GSL.SP.1999.156.01.12}, journal-iso = {GEOL SOC SPEC PUBL}, journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS}, volume = {156}, unique-id = {1256307}, issn = {0305-8719}, abstract = {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.}, year = {1999}, eissn = {2041-4927}, pages = {215-250}, orcid-numbers = {Lenkey, László/0000-0003-4236-4075} } @article{MTMT:1635999, title = {Controls on development of Mid-Triassic ramps: examples from southern Hungary}, url = {https://m2.mtmt.hu/api/publication/1635999}, author = {Török, Ákos}, doi = {10.1144/GSL.SP.1999.149.01.16}, journal-iso = {GEOL SOC SPEC PUBL}, journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS}, volume = {149}, unique-id = {1635999}, issn = {0305-8719}, abstract = {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.}, year = {1998}, eissn = {2041-4927}, pages = {339-367}, orcid-numbers = {Török, Ákos/0000-0002-5394-4510} } @article{MTMT:1635955, title = {Triassic ramp evolution, southern Hungary and its similarities to Germano-type Triassic.}, url = {https://m2.mtmt.hu/api/publication/1635955}, author = {Török, Ákos}, journal-iso = {ACTA GEOL HUNG}, journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES}, volume = {40}, unique-id = {1635955}, issn = {0236-5278}, year = {1997}, pages = {367-390}, orcid-numbers = {Török, Ákos/0000-0002-5394-4510} } @article{MTMT:1025533, title = {Triassic facies types, evolution and paleogeographic relations of the Tisza Megaunit}, url = {https://m2.mtmt.hu/api/publication/1025533}, author = {M, Bleahu and Mantea, G and Bordea, S and Panin, S and Stefanescu, M and Sikic, K and Haas, János and Kovács, Sándor and Péró, Csaba and Bérczi-Makk, A and Konrád, Gyula and Nagy, E and Rálisch-Felgenhauer, E and Török, Ákos}, journal-iso = {ACTA GEOL HUNG}, journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES}, volume = {37}, unique-id = {1025533}, issn = {0236-5278}, year = {1994}, pages = {187-234}, orcid-numbers = {Haas, János/0000-0003-0929-8889; Török, Ákos/0000-0002-5394-4510} } @article{MTMT:1255443, title = {TERTIARY EVOLUTION OF THE INTRA-CARPATHIAN AREA - A MODEL}, url = {https://m2.mtmt.hu/api/publication/1255443}, author = {CSONTOS, L and Nagymarosy, András and Horváth, Ferenc and KOVAC, M}, doi = {10.1016/0040-1951(92)90346-8}, journal-iso = {TECTONOPHYSICS}, journal = {TECTONOPHYSICS}, volume = {208}, unique-id = {1255443}, issn = {0040-1951}, abstract = {The Outer Carpathian flysch nappes encircle an Intra-Carpathian domain which can be divided into two megatectonic units (North Pannonian and Tisza) mostly on the basis of contrasting Mesozoic and Palaeogene facies development. We see two major kinematic problems to be solved: (1) The present distribution of the Mesozoic and Palaeogene facies is mosaic-like, and some belts form exotic bodies within realms of Austroalpine affinity. (2) Late Eocene palinspastic reconstruction of the Outer Carpathian flysch nappes suggest, that the entire Intra-Carpathian area must have been located several hundreds of kilometres to the south and to the west of its present position. Neogene extension can account for shortening in the external Carpathian nappes, but is unable to explain Mesozoic facies anomalies and offsets of Palaeogene formations. We suggest that evolution of the Intra-Carpathian area involved first Late Palaeogene-Early Miocene juxtaposition of the North-Pannonian and Tisza megatectonic units, accompanied by the closure of the external Carpathian flysch troughs; thereafter extension of this amalgamated unit occurred, which was compensated by thrusting of flysch nappes onto the European foreland and formation of molasse foredeeps. Eastward escape of the North-Pannonian unit from the Alpine collisional belt involved left lateral shear along the Pieniny Klippen belt and right lateral shear along the Mid-Hungarian zone. Parts of the Late Palaeogene basin and an Early Miocene volcanic edifice were dissected, offset and elongated by several 100 kms. The driving mechanism of the eastward escape of the Intra-Carpathian area can be related to the collision of Apulia and Europe and the subduction of the external Carpathian crust under the Pannonian units. The escape ceased gradually in the Early Miocene, when oblique collision between the North-Pannonian unit and European continent occurred. Neogene extension of the Pannonian region was an areal deformation. The extension at locally variable rate resulted in the break-up of the heterogenous floor of the Neogene basin. The driving mechanism of basin extension and contemporaneous compressional deformation of the external Carpathians is thought to be related to ongoing subduction, involving the marginal part of the attenuated European continental crust. Tectonic activity in the Carpathians and basin subsidence and volcanism shifted in time and in unison from the west toward the east-southeast.}, year = {1992}, eissn = {1879-3266}, pages = {221-241} } @article{MTMT:1109927, title = {Thermal history of Mesozoic basement in Pannonian Basin (S-Hungary)}, url = {https://m2.mtmt.hu/api/publication/1109927}, author = {Póka, Teréz and Árkai, Péter and Sajgó, Csanád and Horváth, Z A and Tóth, Mária and Völgyi, L}, journal-iso = {ACTA GEOL ACAD SCI HUNG}, journal = {ACTA GEOLOGICA ACADEMIAE SCIENTARIUM HUNGARICAE}, volume = {30}, unique-id = {1109927}, issn = {0001-5695}, year = {1987}, pages = {197-229} }