@article{MTMT: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}, title = {Processes and controlling factors of polygenetic dolomite formation in the Transdanubian Range, Hungary: a synopsis}, 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} } @article{MTMT:2922731, author = {Danišík, M and Fodor, László and Dunkl, I and Gerdes, A and Csizmeg, János and Hámorné, Vidó Mária and Evans, NJ}, doi = {10.1111/ter.12155}, title = {A multi-system geochronology in the Ad-3 borehole, Pannonian Basin (Hungary) with implications for dating volcanic rocks by low-temperature thermochronology and for interpretation of (U-Th)/He data}, journal-iso = {TERRA NOVA}, journal = {TERRA NOVA}, volume = {27}, unique-id = {2922731}, issn = {0954-4879}, year = {2015}, eissn = {1365-3121}, pages = {258-269} } @article{MTMT:2048753, author = {Haas, János and Budai, Tamás and Raucsik, Béla}, doi = {10.1016/j.palaeo.2012.06.031}, title = {Climatic controls on sedimentary environments in the Triassic of the Transdanubian Range (Western Hungary)}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {353-355}, unique-id = {2048753}, issn = {0031-0182}, year = {2012}, eissn = {1872-616X}, pages = {31-44}, orcid-numbers = {Haas, János/0000-0003-0929-8889; Raucsik, Béla/0000-0002-1951-5974} } @article{MTMT:152141, author = {Hips, Kinga and Haas, János}, doi = {10.1007/s10347-009-0182-8}, title = {Facies and diagenetic evaluation of the Permian-Triassic boundary interval and basal Triassic carbonates: shallow and deep ramp sections, Hungary.}, journal-iso = {FACIES}, journal = {FACIES}, volume = {55}, unique-id = {152141}, issn = {0172-9179}, year = {2009}, pages = {421-442}, orcid-numbers = {Hips, Kinga/0000-0003-2315-120X; Haas, János/0000-0003-0929-8889} } @article{MTMT:1236932, author = {Csontos, L and Vörös, Attila}, doi = {10.1016/j.palaeo.2004.02.033}, title = {Mesozoic plate tectonic reconstruction of the carpathian region}, 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:1019032, author = {Haas, János and Budai, Tamás}, title = {Triassic sequence stratigraphy of the Transdanubian Range (Hungary)}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {50}, unique-id = {1019032}, issn = {1335-0552}, year = {1999}, pages = {459-475}, orcid-numbers = {Haas, János/0000-0003-0929-8889} } @article{MTMT:1019016, author = {Haas, János and Kovács, Sándor and L, Krystyn and R, Lein}, doi = {10.1016/0040-1951(94)00157-5}, title = {Significance of Late Permian-Triassic facies zones in terrane reconstructions in the Alpine North Pannonian domain}, journal-iso = {TECTONOPHYSICS}, journal = {TECTONOPHYSICS}, volume = {242}, unique-id = {1019016}, issn = {0040-1951}, year = {1995}, pages = {19-40}, orcid-numbers = {Haas, János/0000-0003-0929-8889} } @article{MTMT:1255443, author = {CSONTOS, L and Nagymarosy, András (1949-2016) and Horváth, Ferenc and KOVAC, M}, doi = {10.1016/0040-1951(92)90346-8}, title = {TERTIARY EVOLUTION OF THE INTRA-CARPATHIAN AREA - A MODEL}, 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}, pages = {221-241} }