TY - CONF AU - Márton Péterné Szalay, Emőke AU - Haas, János AU - Fodor, László AU - Velki, Máté AU - Imre, G TI - The Transdanubian Range unit, a far travelled fragment of Adria: quality-controlled Mesozoic paleomagnetic results and their tectonic interpretation in the Adria – Africa geodynamic system T2 - 19th meeting of the Central European Tectonic Studies Group (CETeG) PY - 2023 SP - 61 EP - 62 PG - 2 UR - https://m2.mtmt.hu/api/publication/34541617 ID - 34541617 LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke TI - Hungarian contribution to palaeomagnertism and magnetic anisotropy (2019-2022) - IAGA Division I – Part I. JF - GEOMATIKAI KÖZLEMÉNYEK / PUBLICATIONS IN GEOMATICS J2 - GEOMAT KÖZL VL - 25 PY - 2022 SP - 51 EP - 54 PG - 4 SN - 1419-6492 UR - https://m2.mtmt.hu/api/publication/34410551 ID - 34410551 LA - English DB - MTMT ER - TY - CHAP AU - Cseri, Zoltán AU - Márton Péterné Szalay, Emőke AU - Palotai, Márton AU - Hencz, Mátyás AU - Biró, Tamás AU - Karátson, Dávid ED - Natália, Hudáčková ED - Andrej, Ruman ED - Michal, Šujan TI - Integrating field volcanology, paleomagnetism and structural geology to correlate a poorly preserved Miocene succession in the East Mátra Mts. (Hungary) T2 - Environmental, Structural and Stratigraphical Evolution of the Western Carpathians : Abstract Book PB - Comenius University in Bratislava CY - Pozsony SN - 9788022355193 PY - 2022 SP - 47 EP - 48 PG - 2 UR - https://m2.mtmt.hu/api/publication/33533651 ID - 33533651 LA - English DB - MTMT ER - TY - JOUR AU - Ćosović, Vlasta AU - Imre, Gábor AU - Velki, Máté AU - Márton Péterné Szalay, Emőke TI - Changing directions of the tectonic structures, consistent paleomagnetic directions at the NE imbricated margin of Stable Adria JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 843 PY - 2022 SN - 0040-1951 DO - 10.1016/j.tecto.2022.229594 UR - https://m2.mtmt.hu/api/publication/33140086 ID - 33140086 N1 - Paleomagnetic Laboratory, Department of Geophysical Research, Szabályozott Tevékenységek Felügyeleti Hatósága, Columbus 17-23, Budapest, 1145, Hungary Department of Geology, Faculty of Science, University of Zagreb, Horvatovac 102b, Zagreb, 10000, Croatia Department of Geophysics and Space Science, Eötvös Loránd University. Pázmány Péter 1/C, Budapest, 1117, Hungary Export Date: 24 October 2022 Correspondence Address: Márton, E.; Paleomagnetic Laboratory, Szabályozott Tevékenységek Felügyeleti Hatósága, Columbus 17-23, Hungary; email: paleo@sztfh.hu LA - English DB - MTMT ER - TY - JOUR AU - Karátson, Dávid AU - Biró, Tamás AU - Portnyagin, Maxim AU - Kiss, Balázs AU - Paquette, Jean-Louis AU - Cseri, Zoltán AU - Hencz, Mátyás AU - Németh, Károly AU - Lahitte, Pierre AU - Márton Péterné Szalay, Emőke AU - Kordos, László AU - Józsa, Sándor AU - Hably, Lilla AU - Müller, Samuel TI - Large-magnitude (VEI ≥ 7) ‘wet’ explosive silicic eruption preserved a Lower Miocene habitat at the Ipolytarnóc Fossil Site, North Hungary JF - SCIENTIFIC REPORTS J2 - SCI REP VL - 12 PY - 2022 IS - 1 SN - 2045-2322 DO - 10.1038/s41598-022-13586-3 UR - https://m2.mtmt.hu/api/publication/32894628 ID - 32894628 N1 - Department of Physical Geography, Eötvös University, Budapest, Hungary GEOMAR Helmholtz Centre for Ocean Research, Kiel, Germany Department of Petrology and Geochemistry, Eötvös University, Budapest, Hungary Laboratoire Magmas et Volcans, Université Clermont Auvergne, Clermont-Ferrand, France School of Agriculture and Environment, Massey University, Palmerston North, New Zealand Institute of Earth Physics and Space Science, Sopron, Hungary Université Paris-Saclay, CNRS, UMR GEOPS, Orsay, 91405, France Mining and Geological Survey of Hungary, Paleomagnetic Laboratory, Budapest, Hungary Eötvös University, Savaria University Centre, Szombathely, Hungary Botanical Department, Hungarian Natural History Museum, Budapest, Hungary Institute of Earth Sciences, Christian-Albrecht University of Kiel, Kiel, Germany Ipolytarnóc Fossils Nature Conservation Area, Ipolytarnóc, Hungary Cited By :2 Export Date: 6 December 2022 Correspondence Address: Karátson, D.; Department of Physical Geography, Hungary; email: karatson.david@ttk.elte.hu AB - During Earth's history, geosphere-biosphere interactions were often determined by momentary, catastrophic changes such as large explosive volcanic eruptions. The Miocene ignimbrite flare-up in the Pannonian Basin, which is located along a complex convergent plate boundary between Europe and Africa, provides a superb example of this interaction. In North Hungary, the famous Ipolytarnoc Fossil Site, often referred to as "ancient Pompeii", records a snapshot of rich Early Miocene life buried under thick ignimbrite cover. Here, we use a multi-technique approach to constrain the successive phases of a catastrophic silicic eruption (VEI >= 7) dated at 17.2 Ma. An event-scale reconstruction shows that the initial PDC phase was phreatomagmatic, affecting >= 1500 km(2) and causing the destruction of an interfingering terrestrial-intertidal environment at Ipolytarnoc. This was followed by pumice fall, and finally the emplacement of up to 40 m-thick ignimbrite that completely buried the site. However, unlike the seemingly similar AD 79 Vesuvius eruption that buried Pompeii by hot pyroclastic density currents, the presence of fallen but uncharred tree trunks, branches, and intact leaves in the basal pyroclastic deposits at Ipolytarnoc as well as rock paleomagnetic properties indicate a low-temperature pyroclastic event, that superbly preserved the coastal habitat, including unique fossil tracks. LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke AU - Pipík, Radovan AU - Starek, Dušan AU - Kovácsi, Erika AU - Vidhya, Marina AU - Świerczewska, Anna AU - Tokarski, Antoni K. AU - Vojtko, Rastislav AU - Schlögl, Silvia TI - Enhancing the reliability of the magnetostratigraphic age assignment of azimuthally nonoriented drill cores by the integrated application of palaeomagnetic analysis, field tests, anisotropy of magnetic susceptibility, and the evolution of the endemic fauna as documented on the upper Miocene limnic deposits of the Turiec Basin (Western Carpathians) JF - AAPG BULLETIN J2 - AAPG BULL VL - 106 PY - 2022 IS - 4 SP - 803 EP - 827 PG - 25 SN - 0149-1423 DO - 10.1306/10042120019 UR - https://m2.mtmt.hu/api/publication/32740125 ID - 32740125 N1 - Palaeomagnetic Laboratory Mining and Geological Survey of Hungary, Budapest, Hungary Earth Science Institute, Slovak Academy of Sciences, Banska Bystrica, Slovakia Faculty of Geology Geophysics and Environmental Protection, AGH University of Science and Technology, Krakow, Poland Institute of Geological Sciences, Research Centre in Krakow, Polish Academy of Sciences, Krakow, Poland Department of Geology and Palaeontology, Faculty of Natural Sciences, Comenius University, Bratislava, Slovakia Export Date: 9 December 2022 CODEN: AABUD LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke AU - Toljić, Marinko AU - Cvetkov, Vesna TI - Late and post-collisional tectonic evolution of the Adria-Europe suture in the Vardar Zone JF - JOURNAL OF GEODYNAMICS J2 - J GEODYN VL - 149 PY - 2022 SN - 0264-3707 DO - 10.1016/j.jog.2021.101880 UR - https://m2.mtmt.hu/api/publication/32552690 ID - 32552690 N1 - Mining and Geological Survey of Hungary, Paleomagnetic Laboratory, Columbus utca 17–23, Budapest, H 1145, Hungary University of Belgrade-Faculty of Mining and Geology, Djušina 7, Belgrade, 11000, Serbia Cited By :1 Export Date: 1 July 2022 Correspondence Address: Márton, E.; Mining and Geological Survey of Hungary, Columbus utca 17–23, Hungary; email: paleo@mbfsz.gov.hu LA - English DB - MTMT ER - TY - CHAP AU - Cseri, Zoltán AU - Hencz, Mátyás AU - Biró, Tamás AU - Márton Péterné Szalay, Emőke AU - Lahitte, P AU - Paquette, JL AU - Karátson, Dávid ED - Király, Edit ED - Füri, Judit TI - A KELET-MÁTRAI KÖZÉPSŐ DÁCITTUFA ÚJ VULKA-NOSZTRATIGRÁFIAI EREDMÉNYEI T2 - Átalakulások II. PB - Magyarhoni Földtani Társulat CY - Budapest SN - 9789638221834 PY - 2021 SP - 17 EP - 17 PG - 1 UR - https://m2.mtmt.hu/api/publication/32212805 ID - 32212805 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Madzin, Jozef AU - Márton Péterné Szalay, Emőke AU - Starek, Dusan AU - Mikus, Tomas TI - Magnetic fabrics in the turbidite deposits of the Central Carpathian Paleogene Basin in relation to sedimentary and tectonic fabric elements JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 72 PY - 2021 IS - 2 SP - 134 EP - 154 PG - 21 SN - 1335-0552 DO - 10.31577/GeolCarp.72.2.4 UR - https://m2.mtmt.hu/api/publication/32059471 ID - 32059471 N1 - Funding Agency and Grant Number: National Development and Innovation Office of Hungary [K128625]; Slovak Research and Development AgencySlovak Research and Development Agency [APVV-0212-12, APVV-17-0170]; VEGA AgencyVedecka grantova agentura MSVVaS SR a SAV (VEGA) [2/0028/17, 2/0014/18, 2/0013/20] Funding text: The study was financially supported by the National Development and Innovation Office of Hungary (project K128625), the Slovak Research and Development Agency (former project APVV-0212-12 and running project APVV-17-0170) and by the VEGA Agency (projects 2/0028/17, 2/0014/18 and 2/0013/20). We thank Tunde Csefan, Gabor Imre, Juraj Surka and several members of my family (JM) for their technical assistance in the field and -laboratory. Thanks to Sergii Kurylo for his help with the SEM analysis. We thank Pablo Calvin, Frantisek Hrouda and Anna Wysocka for their detailed and valuable reviews that helped to improve the first draft. Editorial handling by Jan Sotak is appreciated. AB - Anisotropy of magnetic susceptibility and anisotropy of anhysteretic remanent magnetization were studied in the Oligocene turbidites of the weakly deformed Central Carpathian Paleogene Basin. In order to decide whether the magnetic fabric can be related to deposition from a paleoflow or to incipient weak tectonic deformation we compared magnetic fabrics in individual intervals of the Bouma sequence with sedimentary structures and tectonic brittle mesostructures (joints). In the Ta-Te intervals we observed a good correlation between maximum susceptibility axes and SW(W)-NE(E) oriented paleoflows. Within convoluted and slump folded sandstones the AMS fabric coincides with the orientation of soft-sediment deformation structures. These features suggest the sedimentary origin of the AMS fabric. Three types of AARM sub-fabric were distinguished. The AARM type 1 represents magnetic foliations parallel either to NNW-SSE or to NE-SW oriented joints with magnetic lineations distributed along the joins. In the AARM type 2 magnetic foliations remained parallel to the bedding while magnetic lineations group around the joint to bedding intersections. The AARM type 3 coincides with the AMS fabric. Magnetic and microscopic analyses indicate that the AARM fabrics are connected to magnetite associated with subordinate ferrimagnetic iron sulphides. Both minerals occur in a sub-microscopic size and formed most likely during late diagenesis through the alteration of pyrite, possibly accompanied by burial clay transformation processes. The growth of the authigenic ferrimagnetic minerals was conditioned by combined effects of the sedimentary petrofabric, lithology and stress conditions during the inversion of the basin in the Early to Middle Miocene. LA - English DB - MTMT ER - TY - GEN AU - Biró, Tamás AU - Hencz, Mátyás AU - Németh, Károly AU - Karátson, Dávid AU - Márton Péterné Szalay, Emőke AU - Szakács, Alexandru AU - Bradák, Balázs AU - Szalai, Zoltán AU - Pécskay, Zoltán AU - Kovács, István János TI - Egy Miocén freatopliniuszi kitörés: a "Jató member" fizikai vulkanológiai jellemzői PY - 2021 UR - https://m2.mtmt.hu/api/publication/32014878 ID - 32014878 LA - Hungarian DB - MTMT ER -