@article{MTMT:3097539,
	title = {The link between tectonics and sedimentation in back-arc basins: New genetic constraints from the analysis of the Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/3097539},
	author = {Balázs, Attila and Matenco, L and Magyar, Imre and Horváth, Ferenc and Cloetingh, S},
	doi = {10.1002/2015TC004109},
	journal-iso = {TECTONICS},
	journal = {TECTONICS},
	volume = {35},
	unique-id = {3097539},
	issn = {0278-7407},
	abstract = {The architecture of sedimentary basins reflects the relationship between accommodation space and sediment supply, their rates and localization being variable during basin evolution. The mechanisms driving the interplay between tectonics and sedimentation in extensional back-arc basins overlying rheological weak zones inherited from an earlier orogenic evolution are less understood. A typical example is the Pannonian back-arc basin of Central Europe. It is floored by continental lithosphere and was affected by large amounts of extension driven by the subduction rollback that took place in the Carpathians and/or Dinarides. A novel kinematic and seismic sequence stratigraphic interpretation calibrated by wells allows the quantification of the link between the formation of half grabens and coeval sedimentation in the Great Hungarian Plain part of the basin. While the lower order tectonic-induced cycles characterize the main phases of extension in various subbasins, the higher-order cyclicity and associated unconformities define individual moments of fault (re)activation. Our novel interpretation of a temporal and spatial migration of extension during Miocene times explains the contrasting present-day strike of various subbasins as a result of their gradual clockwise rotation. Incorporating the observed asymmetry, in particular the associated footwall exhumation, infers that the amount of extension is much larger than previously thought. The quantitative link between tectonics and sedimentation has allowed the definition of a novel model of sedimentation in asymmetric basins that can be ported to other natural scenarios of similarly hyperextended back-arc basins observed elsewhere. ©2016. American Geophysical Union. All Rights Reserved.},
	keywords = {STRATIGRAPHY; Pannonian Basin; carpathians; Tectonics; Structural geology; Lithology; Sedimentation; Inversion tectonics; Tectonic system; Back-arc extensions; tectonic system tracts; back-arc extension},
	year = {2016},
	eissn = {1944-9194},
	pages = {1526-1559},
	orcid-numbers = {Balázs, Attila/0000-0003-2948-0397}
}

@{MTMT:3175271,
	title = {Pannonian molluscs and their localities in the Gerecse Hills, Transdanubian Range},
	url = {https://m2.mtmt.hu/api/publication/3175271},
	author = {Magyar, Imre and Sztanó, Orsolya and Csillag, Gábor and Kercsmár, Zsolt and Katona, Lajos Tamás and Lantos, Zoltán and Bartha, István Róbert and Budai, S and Fodor, László},
	booktitle = {Environmental, Structural and stratigraphical Evolution of the Western Carpathians},
	unique-id = {3175271},
	year = {2016},
	pages = {54-55},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653; Bartha, István Róbert/0000-0003-3198-2687}
}

@article{MTMT:3159399,
	title = {Late Miocene sedimentary record of the Danube/Kisalföld Basin: interregional correlation of depositional systems, stratigraphy and structural evolution},
	url = {https://m2.mtmt.hu/api/publication/3159399},
	author = {Sztanó, Orsolya and Kováč, M and Magyar, Imre and Šujan, M and Fodor, László and Uhrin, András and Rybár, S and Csillag, Gábor and Tőkés, Lilla},
	doi = {10.1515/geoca-2016-0033},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {67},
	unique-id = {3159399},
	issn = {1335-0552},
	year = {2016},
	eissn = {1336-8052},
	pages = {525-542},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653; Tőkés, Lilla/0000-0002-2518-9431}
}

@{MTMT:2912997,
	title = {Lake Pannon Deltaic deposits in Gerecse hills, Hungary},
	url = {https://m2.mtmt.hu/api/publication/2912997},
	author = {Bartha, István Róbert and Magyar, Imre and Fodor, László and Csillag, Gábor and Lantos, Zoltán and Tőkés, Lilla and Sztanó, Orsolya},
	booktitle = {Neogene of the Paratethyan Region: 6th Workshop on the Neogene of Central and South-Eastern Europe. An RCMNS Interim Colloquium},
	unique-id = {2912997},
	year = {2015},
	pages = {19-20},
	orcid-numbers = {Bartha, István Róbert/0000-0003-3198-2687; Tőkés, Lilla/0000-0002-2518-9431; Sztanó, Orsolya/0000-0003-0786-3653}
}

@inproceedings{MTMT:2906290,
	title = {Neogene stratigraphy in the Mecsek region. Hetvehely, Badenian rocky shore and fossiliferous shorface sand},
	url = {https://m2.mtmt.hu/api/publication/2906290},
	author = {Sebe, Krisztina and Csillag, Gábor and Dulai, Alfréd and Gasparik, Mihály and Magyar, Imre and Selmeczi, Ildikó and Szabó, Márton and Sztanó, Orsolya and Szuromi-Korecz, A},
	booktitle = {Neogene of the Paratethyan Region: 6th Workshop on the Neogene of Central and South-Eastern Europe. An RCMNS Interim Colloquium},
	unique-id = {2906290},
	year = {2015},
	pages = {102-124},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Sztanó, Orsolya/0000-0003-0786-3653}
}

@article{MTMT:3114745,
	title = {Erratum: Turbidites as indicators of paleotopography, Upper Miocene Lake Pannon, Western Mecsek Mountains (Hungary) (Geologica Carpathica (2015) 66: 4 (331-344) DOI: 10.1515/geoca-2015-0029)},
	url = {https://m2.mtmt.hu/api/publication/3114745},
	author = {Sztanó, Orsolya and Sebe, Krisztina and Csillag, Gábor and Magyar, Imre},
	doi = {10.1515/geoca-2015-0036},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {66},
	unique-id = {3114745},
	issn = {1335-0552},
	year = {2015},
	eissn = {1336-8052},
	pages = {439-439},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653; Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:2934948,
	title = {Turbidites as indicators of paleotopography, Upper Miocene Lake Pannon, Western Mecsek Mountains (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2934948},
	author = {Sztanó, Orsolya and Sebe, Krisztina and Csillag, Gábor and Magyar, Imre},
	doi = {10.1515/geoca-2015-0029},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {66},
	unique-id = {2934948},
	issn = {1335-0552},
	year = {2015},
	eissn = {1336-8052},
	pages = {331-344},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653; Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:2154674,
	title = {Progradation of the paleo-Danube shelf margin across the Pannonian Basin during the Late Miocene and Early Pliocene},
	url = {https://m2.mtmt.hu/api/publication/2154674},
	author = {Magyar, Imre and Radivojević, D and Sztanó, Orsolya and Synak, R and Ujszászi, K and Pócsik, M},
	doi = {10.1016/j.gloplacha.2012.06.007},
	journal-iso = {GLOBAL PLANET CHANGE},
	journal = {GLOBAL AND PLANETARY CHANGE},
	volume = {103},
	unique-id = {2154674},
	issn = {0921-8181},
	abstract = {The basin of giant Lake Pannon in Central Europe was filled by forward accretion of sediment packages during the Late Miocene and Early Pliocene. Successive positions of the shelf-margin are represented by a series of clinoforms in seismic profiles. The height of the clinoforms (and thus the inferred paleo water depth) is 200-600 m in the successions; the width of the slope, measured from the shelf-break down to the toe of slope, varies between 5 and 15 km. Geographical position of successive shelf-margin slopes indicates that about 2/3 of the basin area was filled by sediment transport systems supplying sediments from the NW, from the Alps and Western Carpathians. The first shelf-margin slope was built by the paleo-Danube in the Kisalföld/Danube sub-basin about 10 Ma ago, and during the subsequent 6 Ma it prograded ca. 400 km to the SE across the Pannonian Basin, with an average of 67 km/Ma slope advance. The most significant agent of this shelf growth was the sediment dispersal system of the paleo-Danube, hence we designate this northwestern shelf the paleo-Danube shelf. The northeastern part of Lake Pannon was filled by the paleo-Tisza system, supplying sediments from the Northeastern and Eastern Carpathians. Additional local systems carried sediments from E to W along the eastern margin and S to N along the southern margin of the Pannonian Basin, respectively. The deep-water environment disappeared from the Pannonian Basin and the endemic, brackish biota of Lake Pannon went extinct probably 4 Ma ago, when the paleo-Danube shelf margin and a (yet unidentified) shelf margin prograding in the opposite direction met in the southeastern corner of the Pannonian Basin. © 2012 Elsevier B.V. All rights reserved.},
	keywords = {Pannonian Basin; Lake Pannon; Progradation; Shelf-margin; Paleo-Danube; Clinoform},
	year = {2013},
	eissn = {1872-6364},
	pages = {168-173},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653}
}

@article{MTMT:2498680,
	title = {A Tihanyi Formáció a Balaton környékén: típusszelvény, képződési körülmények, rétegtani jellemzés. Tihany Formation in the surroundings of Lake Balaton: Type locality, depositional setting and stratigraphy},
	url = {https://m2.mtmt.hu/api/publication/2498680},
	author = {Sztanó, Orsolya and Magyar, Imre and Szónoky, Miklós and Lantos, Miklós and Müller, Pál and Lenkey, László and Katona, Lajos Tamás and Csillag, Gábor},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {143},
	unique-id = {2498680},
	issn = {0015-542X},
	abstract = {MatarkaID=1911933},
	year = {2013},
	eissn = {2559-902X},
	pages = {73-98},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653; Lenkey, László/0000-0003-4236-4075}
}

@inbook{MTMT:2145538,
	title = {Biostratigraphy in a late Neogene Caspian-Type Lacustrine Basin: Lake Pannon, Hungary},
	url = {https://m2.mtmt.hu/api/publication/2145538},
	author = {Magyar, Imre and Geary, DH},
	booktitle = {Lacustrine sandstone reservoirs and hydrocarbon systems},
	doi = {10.1306/13291392M953142},
	unique-id = {2145538},
	year = {2012},
	pages = {255-264}
}

@article{MTMT:1354802,
	title = {Fiatal tektonikai jelenségek új észlelései a Nyugati-Mecsekben és környezetében},
	url = {https://m2.mtmt.hu/api/publication/1354802},
	author = {Konrád, Gyula and Sebe, Krisztina},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {140},
	unique-id = {1354802},
	issn = {0015-542X},
	abstract = {Exposures of Neogene and Quaternary age were investigated along the main structural zones of the Western Mecsek
		Mts. (SW Hungary) in order to study post-Miocene tectonic activity, with an aim of supplementing studies on the longterm
		stability of the region. Field observations showed that young movements affected only the mountain fronts and the
		foreland. From the 24 studied exposures, those with impacts of tectonic activity were located along the major fault zones
		of the Western Mecsek Mts. and prove tectonic/seismic events occurring as late as the Late Pleistocene along the
		Mecsekalja Dislocation Zone and probably the Hetvehely–Magyarszék Fault. On the contrary, no impact of neotectonic
		activity was found within the Western Mecsek Anticline, indicating that this area behaved as a single solid block during
		post-Miocene movements. Since the Karpatian age, 5 tectonic phases could be distinguished. From these – somewhat
		opposing previous research – transtension seems typical for the Karpatian along the Hetvehely–Magyarszék Fault. The
		Early Pannonian transtensional stress field did not cease to exist at the beginning of the Late Pannonian. Tectonic
		inversion started only within the first half of the Late Pannonian and can be considered active up to present day in the
		major part of the area.
		
		A munka során a Nyugat-Mecsek fő szerkezeti vonalainak környezetében feltárt neogén és kvarter képződményeket
		vizsgáltuk fiatal (posztpannóniai) tektonikai aktivitás nyomai után kutatva, elsősorban a terület hosszú távú
		stabilitásának megítéléséhez. A terepi megfigyelések alapján a fiatal mozgások csak a hegységperemet és az előteret
		érintették. A vizsgált 24 feltárásból a fiatal tektonikával érintettek a Nyugat-Mecsek meghatározó szerkezeti vonalai
		mentén helyezkednek el, és még a késő-pleisztocénben is szerkezeti mozgásokat, illetve szeizmikus aktivitást
		bizonyítanak a Mecsekalja-öv és valószínűleg a Hetvehely–magyarszéki-törés mentén. Ezzel ellentétben a Nyugatmecseki-
		antiklinális területén belül neotektonikára utaló jeleket nem észleltünk, ez alapján a pannóniai–negyedidőszaki
		mozgások során a Nyugat-Mecsek egységes tömbként viselkedhetett.
		A kárpáti korszak óta öt tektonikai fázis volt elkülöníthető a területen. Ezek közül – a korábbi vizsgálati
		eredményekkel szemben – a kárpáti korszakra jellemzőnek tűnik a transztenzió a Hetvehely–magyarszéki-törés
		mentén. A kora-pannóniai transztenziós feszültségtér a Mecsekalja-öv mentén még a késő-pannóniai elején is
		fennállt. Az inverzió a késő-pannóniai első felében kezdődött és a terület legnagyobb részén máig aktívnak
		tekinthető.},
	year = {2010},
	eissn = {2559-902X},
	pages = {135-161},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1333817,
	title = {Life in the sublittoral zone of long-lived Lake Pannon: paleontological analysis of the Upper Miocene Szak Formation, Hungary. Paleontological analysis of the Upper Miocene Szák Formation, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1333817},
	author = {Cziczer, István and Magyar, Imre and Pipik, R and Bohme, M and Coric, S and Bakrac, K and Suto-Szentai, M and Lantos, M and Babinszki, Edit and Muller, P},
	doi = {10.1007/s00531-008-0322-3},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {98},
	unique-id = {1333817},
	issn = {1437-3254},
	abstract = {Life and depositional environments in the sublittoral zone of Lake Pannon, a large, brackish Paratethyan lake from the Late Miocene, were reconstructed from fossils and facies of the Szak Formation. This formation is exposed in several, roughly coeval (9.4-8.9 Ma) outcrops, located along strike of the paleo-shelf-break in northwestern Hungary. The silty argillaceous marl of the formation was deposited below storm wave base, at 20-30 to 80-90 m water depth. The abundance of benthic organisms indicates that the bottom water was usually well oxygenated. Interstitial dysoxia, however, may have occurred immediately below the sediment-water interface, as evidenced by occasional preservation of trace fossils such as Diplocraterion. The fauna comprised endemic mollusks, including brackish cockles of the subfamily Lymnocardiinae, dreissenid mussels (Congeria), and highly adapted, uniquely large-sized deep-water pulmonate snails (planorbids and lymnaeids). Ostracods were dominated by endemic species and, in some cases, endemic genera of candonids, leptocytherids, cypridids, and loxoconchids. Fish remnants include a sciaenid otolith and the oldest skeletal occurrence of Perca in Europe. The phytoplankton comprised exclusively endemic coccolithophorids, mostly endemic dinoflagellates (prevailingly Spiniferites), and cosmopolitan green algae. The Late Miocene fauna and flora of Lake Pannon were in many ways similar to the modern Caspian biota, and in particular cases can be regarded as its precursor.},
	year = {2009},
	eissn = {1437-3262},
	pages = {1741-1766}
}

@article{MTMT:3189094,
	title = {Constraints on Miocene oceanography and climate in the Western and Central Paratethys: O-, Sr-, and Nd-isotope compositions of marine fish and mammal remains},
	url = {https://m2.mtmt.hu/api/publication/3189094},
	author = {Kocsis, László and Vennemann, TW and Hegner, E and Fontignie, D and Tütken, T},
	doi = {10.1016/j.palaeo.2008.10.003},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {271},
	unique-id = {3189094},
	issn = {0031-0182},
	abstract = {The Paratethys evolved as a marginal sea during the Alpine-Himalayan orogeny in the Oligo-Miocene. Sediments from the northern Alpine Molasse Basin, the Vienna, and the Pannonian Basins located in the western and central part of the Paratethys thus provide unique information on regional changes in climate and oceanography during a period of active Alpine uplift. Oxygen isotope compositions of well-preserved phosphatic fossils recovered from the sediments support deposition under sub-tropical to warm-temperate climate with water temperatures of 14 to 28 °C for the Miocene. δ18O values of fossil shark teeth are similar to those reported for other Miocene marine sections and, using the best available estimates of their biostratigraphic age, show a variation until the end of the Badenian similar to that reported for composite global record. The 87Sr/86Sr isotope ratios of the fossils follow the global Miocene seawater trend, albeit with a much larger scatter. The deviations of 87Sr/86Sr in the samples from the well-constrained seawater curve are interpreted as due to local input of terrestrially-derived Sr. Contribution of local sources is also reflected in the εNd values, consistent with input from ancient crystalline rocks (e.g., Bohemian Massif) and/or Mesozoic sediments with εNd < - 9. On the other hand, there is evidence for input from areas with Neogene volcanism as suggested by samples with elevated εNd values > - 7. Excluding samples showing local influence on the water column, an average εNd value of - 7.9 ± 0.5 may be inferred for the Miocene Paratethys. This value is indistinguishable from the εNd value of the contemporaneous Indian Ocean, supporting a dominant role of this ocean in the Western and Central Paratethys. © 2008 Elsevier B.V. All rights reserved.},
	keywords = {OXYGEN; ISOTOPES; Mammalia; Miocene; Neodymium; tooth; Strontium; Isotopic composition; paleoclimate; oxygen isotope; fossil record; molasse; palaeoceanography; Paratethys; shark; Chondrichthyes; palaeoclimate; paleoceanography; Alpine orogeny; marine mammal; strontium isotope; neodymium isotope; Himalayan orogeny; Mammal remains; Shark teeth},
	year = {2009},
	eissn = {1872-616X},
	pages = {117-129}
}

@article{MTMT:2899890,
	title = {Tertiary deformation history from seismic section study and fault analysis in a former European Tethyan margin (the Mecsek-Villany area, SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2899890},
	author = {Csontos, László and Benkovics, L and Bergerat, F and Mansy, JL and Worum, G},
	doi = {10.1016/S0040-1951(02)00363-3},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {357},
	unique-id = {2899890},
	issn = {0040-1951},
	abstract = {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.},
	year = {2002},
	eissn = {1879-3266},
	pages = {81-102}
}

@inbook{MTMT:1369059,
	title = {Tertiary tectonic evolution of the Pannonian Basin system and neighbouring orogens: a new synthesis of palaeostress data},
	url = {https://m2.mtmt.hu/api/publication/1369059},
	author = {Fodor, László and Csontos, L and Bada, G and Györfi, I and Benkovics, L},
	booktitle = {The Mediterranean Basins: tertiary extension within the Alpine Orogen},
	doi = {10.1144/GSL.SP.1999.156.01.15},
	unique-id = {1369059},
	year = {1999},
	pages = {295-334}
}

@article{MTMT:2176407,
	title = {IBS Pannonian Basin project: a review of the main results and their bearings on hydrocarbon exploration},
	url = {https://m2.mtmt.hu/api/publication/2176407},
	author = {Horváth, Ferenc and Tari, Gábor},
	doi = {10.1144/GSL.SP.1999.156.01.11},
	journal-iso = {GEOL SOC SPEC PUBL},
	journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS},
	volume = {156},
	unique-id = {2176407},
	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 IBS Pannonian Basin project presents a good example of fruitful joint activity between Hungarian and other European scientists, and beneficial co-operation of academia and the petroleum industry. This allowed us to achieve significant progress in the understanding of the structure, tectonic evolution, stratigraphic features and hydrocarbon generation in the Pannonian Basin. The Pannonian region has been an integral part of the Alpine belt, and it reveals the complexity of orogenic evolution. Continental to oceanic rifting, followed by convergence, subduction and continental collision shaped the Palaeozoic-Mesozoic substrata of the region. Subsequently, two periods of basin formation (Late Cretaceous and Palaeogene) occurred, most probably in compressional setting. From the earliest Miocene large scale lateral displacement and block rotation took place in the internal domain of the orogen, together with the formation of the Pannonian Basin. This has been characterized by lithospheric extension, however, interrupted by compressional events. The modern Pannonian Basin is in an initial phase of positive structural inversion. All of these tectonic events had significant impacts on the formation and the economic value of the various petroleum systems in the area.},
	keywords = {Europe; extensional tectonics; basin evolution; tectonic evolution; hydrocarbon exploration; Alpine orogeny},
	year = {1999},
	eissn = {2041-4927},
	pages = {195-213}
}

@article{MTMT:1890263,
	title = {Paleogeographic evolution of the Late Miocene Lake Pannon in Central Europe},
	url = {https://m2.mtmt.hu/api/publication/1890263},
	author = {Magyar, Imre and Geary, DH and Muller, P},
	doi = {10.1016/S0031-0182(98)00155-2},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {147},
	unique-id = {1890263},
	issn = {0031-0182},
	abstract = {The paleogeographic evolution of Lake Pannon within the Pannonian basin is reconstructed with eight maps, ranging from the Middle Miocene to the Early Pliocene. The maps are based on the distribution of selected biozones and specific fossils, and on complementary sedimentological and seismic information. Our reconstruction shows that the history of Lake Pannon can be divided into three distinct intervals: an initial stage with low water level, which resulted in isolation from the sea at about 12 Ma and might have led to temporary fragmentation of the lake; an interval of gradual transgression lasting until ca. 9.5 Ma; and a long late interval of shrinkage and infilling of sediments that persisted into the Early Pliocene. The deep subbasins of the lake formed during the transgressive interval, in more basinward locations than the deep basins of the preceding Sarmatian age. The southern shoreline, running parallel with the Sava and Danube rivers along the northern foot of the Dinarides, changed very Little during the Lifetime of the lake, while the northern shoreline underwent profound changes. (C) 1999 Elsevier Science B.V. All rights reserved.},
	keywords = {BASIN; Pannonian Basin; Neogene; Lakes; paleogeography; Paratethys; biogeography},
	year = {1999},
	eissn = {1872-616X},
	pages = {151-167}
}

@article{MTMT:1255454,
	title = {Stress-induced late-stage subsidence anomalies in the Pannonian basin},
	url = {https://m2.mtmt.hu/api/publication/1255454},
	author = {Horváth, Ferenc and Cloetingh, S},
	doi = {10.1016/S0040-1951(96)00194-1},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {266},
	unique-id = {1255454},
	issn = {0040-1951},
	abstract = {Subsidence, sedimentation and tectonic quiescence of the Pannonian
		basin was interrupted a few million years ago by tectonic reactivation.
		This recent activity has manifested itself in uplift of the western and
		eastern flanks, and continuing subsidence of the central part of the
		Pannonian basin. Low- to medium-magnitude earthquakes of the
		Carpathian-Pannonian region are generated mostly in the upper crust by
		reverse and wrench fault mechanisms. There is no evidence for
		earthquakes of extensional origin.
		2-D model calculation of the subsidence history shows that a recent
		increase in magnitude of horizontal compressional intraplate stress can
		explain fairly well the observed Quaternary uplift and subsidence
		pattern. We propose that this stress increase is caused by the overall
		Europe/Africa convergence. In Late Pliocene, consumption of subductible
		lithosphere at the eastern margin of the Pannonian basin was completed,
		and the lithosphere underlying the Pannonian basin became locked in a
		stable continental frame. Consequently extensional basin formation has
		come to an end, and compressional inversion of the Pannonian basin is
		in progress.},
	year = {1996},
	eissn = {1879-3266},
	pages = {287-300}
}

@article{MTMT:1255444,
	title = {Styles of extension in the Pannonian Basin.},
	url = {https://m2.mtmt.hu/api/publication/1255444},
	author = {Tari, Gábor and Horváth, Ferenc and RUMPLER, J},
	doi = {10.1016/0040-1951(92)90345-7},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {208},
	unique-id = {1255444},
	issn = {0040-1951},
	abstract = {Structural interpretation of reflection seismic profiles reveals distinct modes of upper crustal extension in the Pannonian Basin. While some subbasins in the Pannonian Basin complex show little extension (planar rotational normal faults), others are characterized by large magnitude of extension (detachment faults, metamorphic core complexes). Gravitational collapse of the Intra-Carpathian domain, combined with subduction zone roll-back is thought to be the driving mechanism of the Neogene back-arc extension.
		
		The very heterogeneously distributed extension is accommodated by transfer faults, which bound regions characterized by different polarity, direction, or amount of extension. In cross section these transfer faults are characterized by flower structures, typical for strike-slip faults.
		
		Seismic stratigraphic interpretations indicate that the non-marine post-rift sedimentary fill of the Pannonian Basin can be described in terms of sequence stratigraphy. The exceptionally good seismic sequence resolution allows recognition of third-order and also fourth-order depositional sequences, which may reflect the interplay of tectonics and eustasy, and Milankovitch scale climatic variations, respectively.},
	year = {1992},
	eissn = {1879-3266},
	pages = {203-219}
}