@article{MTMT:31950068,
	title = {Fluvial magnetic susceptibility as a proxy for long‐term variations of mountain permafrost development in the Alp‐Carpathian region},
	url = {https://m2.mtmt.hu/api/publication/31950068},
	author = {Püspöki, Zoltán and Gibbard, PL and Nádor, A and Thamóné Bozsó, Edit and Sümegi, Pál and Fogarassy-Pummer, Tímea and McIntosh, Richard William and Lantos, M and Tóth‐Makk, Á and Stercel, F and Krassay, Z and Kovács, Péter Gábor and Szőcs, Teodóra and Fancsik, Tamás},
	doi = {10.1111/bor.12520},
	journal-iso = {BOREAS},
	journal = {BOREAS},
	volume = {50},
	unique-id = {31950068},
	issn = {0300-9483},
	keywords = {földtan},
	year = {2021},
	eissn = {1502-3885},
	pages = {806-825},
	orcid-numbers = {Püspöki, Zoltán/0000-0002-8282-7620; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:31621407,
	title = {High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data},
	url = {https://m2.mtmt.hu/api/publication/31621407},
	author = {Püspöki, Zoltán and Fogarassy-Pummer, Tímea and Thamóné Bozsó, Edit and Falus, György and Cserkész-Nagy, Ágnes and Szappanos, B and Márton Péterné Szalay, Emőke and Lantos, Zoltán and Szabó, Szilárd and Stercel, F and Tóth‐Makk, Á and McIntosh, Richard William and Szőcs, Teodóra and Pálóczy, P and Fancsik, Tamás},
	doi = {10.1111/bor.12471},
	journal-iso = {BOREAS},
	journal = {BOREAS},
	volume = {50},
	unique-id = {31621407},
	issn = {0300-9483},
	keywords = {Duna-Tisza köze; földtan},
	year = {2021},
	eissn = {1502-3885},
	pages = {205-223},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867; Szabó, Szilárd/0000-0002-2670-7384}
}

@techreport{MTMT:31991821,
	title = {HGFO–9 Paleoklíma változások kimutatás ásványtan-geokémiai módszerekkel},
	url = {https://m2.mtmt.hu/api/publication/31991821},
	author = {Fogarassy-Pummer, Tímea and Cserkész-Nagy, Ágnes and Thamóné Bozsó, Edit and Kónya, Péter and Markos, Gábor and Demény, K. and Pálfi, É and Tihanyiné, Szép E. and Angyal, J. and Szőcs, Teodóra and Báthori, I.-né},
	editor = {Püspöki, Zoltán},
	unique-id = {31991821},
	keywords = {földtan},
	year = {2020},
	pages = {1-72}
}

@article{MTMT:30829948,
	title = {High‐resolution stratigraphy of a Quaternary fluvial deposit based on magnetic susceptibility variations (Jászság Basin, Hungary).},
	url = {https://m2.mtmt.hu/api/publication/30829948},
	author = {Püspöki, Zoltán and Fogarassy-Pummer, Tímea and Thamóné Bozsó, Edit and Berényi, Bernadett and Cserkész-Nagy, Ágnes and Szappanos, B and Márton Péterné Szalay, Emőke and Lantos, Zoltán and Nádor, Annamária and Fancsik, Tamás and Stercel, F and Tóth‐Makk, Á and McIntosh, Richard William and Szőcs, Teodóra and Faragó, Enikő},
	doi = {10.1111/bor.12412},
	journal-iso = {BOREAS},
	journal = {BOREAS},
	volume = {49},
	unique-id = {30829948},
	issn = {0300-9483},
	abstract = {Quaternary fluvial succession of the Jaszsag Basin (Hungary) was investigated, challenging the stratigraphical potential of 'early postglacial fluvial magnetic susceptibility episodes' recognized earlier in the Koros Basin. Low field magnetic susceptibility (MS) was measured in four boreholes from the basin centre and margins, representing channel and flood-plain environments. Statistical distributions of MS data contain significant sets of outliers, regardless of facies conditions. The downhole distribution of these outliers produces magnetic susceptibility cycles. Supported by magnetic susceptibility cycles, high-resolution facies correlations were performed reflecting a steady palaeohydrographical situation in the area, with a trunk river to the southeast and tributaries to the northwest. SEM-EDX data revealed that ferromagnetic grains are responsible for the outlying MS values. The heterogeneous association of magnetite indicates a catchment area with volcanic and metamorphic rocks, while the group of small (<5 mu m) magnetite octahedrons originated from nearby rhyolitic tuff formations. Magnetic grains were transported along channel belts, while small (<2 mu m) magnetic particles were floated onto flood-plains attached to clays. Climatic control is indicated by peaks at similar to 100 ka frequency in spectra of MS records and was also detected in palaeosol development and in flood frequency using the spectra of measured colour (similar to 100 ka) and logged resistivity (similar to 100 ka, similar to 41 ka), respectively. The climate-dependent MS signal traceable far into the basin in both channel and flood-plain environments can be summoned when the Quaternary fluvial succession of the Pannonian Basin is investigated, assuming some sources of magnetite in the catchment areas. According to the concept of 'fluvial magnetic susceptibility episodes', the early postglacial escape and spreading of the magnetite fraction control the MS signal that can support mapping of the unconformable Quaternary base and building of high-resolution models of aquifers.},
	keywords = {Magnetic susceptibility; Jászság; geológia; földtan},
	year = {2020},
	eissn = {1502-3885},
	pages = {181-199},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@techreport{MTMT:31991815,
	title = {Jelentés az ivó és öntözővizes rétegsor nagy felbontású fácies korrelációs vizsgálatairól debrecen-dél területen különös tekintettel a hidrodinamikai és transzportmodellek gyakorlati szempontjaira},
	url = {https://m2.mtmt.hu/api/publication/31991815},
	author = {Fogarassy-Pummer, Tímea and Markos, Gábor and Gál, Nóra Edit},
	editor = {Püspöki, Zoltán},
	unique-id = {31991815},
	keywords = {geológia; földtan},
	year = {2019},
	pages = {1-50}
}

@{MTMT:30324622,
	title = {2. Módszertani fejlesztési lehetőségek a hazai szénkutatási gyakorlatban},
	url = {https://m2.mtmt.hu/api/publication/30324622},
	author = {Püspöki, Zoltán and Fogarassy-Pummer, Tímea and Cserkész-Nagy, Ágnes and Markos, Gábor},
	booktitle = {A hazai szénvagyon és hasznosítási lehetőségei},
	unique-id = {30324622},
	year = {2018},
	pages = {21-27}
}

@CONFERENCE{MTMT:31289168,
	title = {Coastal effects in East-Borsod Basin presented by high resolution stratigraphic correlation.},
	url = {https://m2.mtmt.hu/api/publication/31289168},
	author = {Fogarassy-Pummer, Tímea and SÁRI, K. and BUDAY-BÓDI, E. and KERTÉSZ, T.},
	booktitle = {XLVII. Ifjú Szakemberek Ankétja – Meeting of Young Geoscientists, Tiszafüred, 01–02/04/2016. Absztraktkötet},
	unique-id = {31289168},
	year = {2016},
	pages = {37-38}
}