@article{MTMT:32475967,
	title = {From marginal outcrops to basin interior: a new perspective on the sedimentary evolution of the eastern Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/32475967},
	author = {Bartha, István Róbert and Botka, Dániel Bálint and Beliczainé Csoma, Vivien and Katona, Lajos Tamás and Tóth, Emőke and Magyar, Imre and Silye, Lóránd and Sztanó, Orsolya},
	doi = {10.1007/s00531-021-02117-6},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {111},
	unique-id = {32475967},
	issn = {1437-3254},
	year = {2022},
	eissn = {1437-3262},
	pages = {335-357},
	orcid-numbers = {Bartha, István Róbert/0000-0003-3198-2687; Botka, Dániel Bálint/0000-0002-6627-4640; Beliczainé Csoma, Vivien/0000-0002-2593-5537; Tóth, Emőke/0000-0002-1733-7828; Silye, Lóránd/0000-0001-7306-6041; Sztanó, Orsolya/0000-0003-0786-3653}
}

@article{MTMT:32533253,
	title = {Sarmatian and Pannonian mollusks from Pécs-Danitzpuszta, southern Hungary: a unique local faunal succession},
	url = {https://m2.mtmt.hu/api/publication/32533253},
	author = {Botka, Dániel Bálint and Rofrics, N and Katona, Lajos Tamás and Magyar, Imre},
	doi = {10.23928/foldt.kozl.2021.151.4.335},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {151},
	unique-id = {32533253},
	issn = {0015-542X},
	year = {2021},
	eissn = {2559-902X},
	pages = {335-361},
	orcid-numbers = {Botka, Dániel Bálint/0000-0002-6627-4640}
}

@article{MTMT:32525530,
	title = {An exceptional surface occurrence: the middle to upper Miocene succession of Pécs-Danitzpuszta (SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/32525530},
	author = {Sebe, Krisztina and Konrád, Gyula and Sztanó, Orsolya},
	doi = {10.23928/foldt.kozl.2021.151.3.235},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {151},
	unique-id = {32525530},
	issn = {0015-542X},
	year = {2021},
	eissn = {2559-902X},
	pages = {235-252},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Sztanó, Orsolya/0000-0003-0786-3653}
}

@article{MTMT:32461594,
	title = {Lake Pannon Transgression on the Westernmost Tip of the Carpathians Constrained by Biostratigraphy and Authigenic 10be/9be Dating (Central Europe)},
	url = {https://m2.mtmt.hu/api/publication/32461594},
	author = {Šujan, M and Braucher, R and Mandic, O and Fordinál, K and Brixová, B and Pipík, RK and Šimo, V and Jamrich, M and Rybár, S and Klučiar, T and Ruman, A and Zvara, I and Kováč, M and Aster, Team},
	doi = {10.13130/2039-4942/16620},
	journal-iso = {RIV IT PALEON STRATIG},
	journal = {RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA},
	volume = {127},
	unique-id = {32461594},
	issn = {0035-6883},
	year = {2021},
	eissn = {2039-4942},
	pages = {627-653}
}

@article{MTMT:30486908,
	title = {The Sarmatian/Pannonian boundary at the western margin of the Vienna Basin (City of Vienna, Austria)},
	url = {https://m2.mtmt.hu/api/publication/30486908},
	author = {Harzhauser, Mathias and Mandic, Oleg and Kranner, Matthias and Lukeneder, Petra and Kern, Andrea K. and Gross, Martin and Carnevale, Giorgio and Jawecki, Christine},
	doi = {10.17738/ajes.2018.0003},
	journal-iso = {AUST J EARTH SCI},
	journal = {AUSTRIAN JOURNAL OF EARTH SCIENCES},
	volume = {111},
	unique-id = {30486908},
	issn = {0251-7493},
	abstract = {Sarmatian and Pannonian cores, drilled at the western margin of the Vienna Basin in the City of Vienna, reveal a complex succession of marine and lacustrine depositional environments during the middle to late Miocene transition. Two Sarmatian and two Pannonian transgressive-regressive sequences were studied in detail. Identical successions of benthic faunal assemblages and similar patterns in magnetic susceptibility logs characterise these sequences. This allows a correlation of the boreholes over a distance of similar to 3.5 km across one of the major marginal faults of the Vienna Basin. Biostratigraphic data, combined with rough estimates of sedimentation rates, reveal large gaps between these sequences, suggesting that only major transgressions reached this marginal area. In particular, during the Sarmatian-Pannonian transition, the basin margin completely emerged and turned into a terrestrial setting for at least 600 ka.},
	keywords = {Miocene; Vienna Basin; Lake Pannon; Paratethys Sea; authigenic pyrite},
	year = {2018},
	eissn = {2072-7151},
	pages = {26-+}
}