TY - CHAP AU - Ozsvárt, Péter AU - Vető, István AU - Nagymarosy, András ED - Bosnakoff, Mariann ED - Főzy, István TI - A paleogén-medence fejlődése a korai oligocénben mikropaleontológiai és geokémiai adatok tükrében T2 - 22. Magyar Őslénytani Vándorgyűlés, Döbrönte. Program, előadáskivonatok, kirándulásvezető PB - Magyarhoni Földtani Társulat CY - Budapest SN - 9789638221759 PY - 2019 SP - 28 EP - 28 PG - 1 UR - https://m2.mtmt.hu/api/publication/31971213 ID - 31971213 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Bakacsi, Zsófia AU - Koós, Sándor AU - Nagymarosy, András AU - László, Péter TI - Riolittufa mállásának hatása a talajok vízvezető képességére JF - AGROKÉMIA ÉS TALAJTAN J2 - AGROKÉMIA ÉS TALAJTAN VL - 65 PY - 2016 IS - 1 SP - 5 EP - 15 PG - 11 SN - 0002-1873 DO - 10.1556/0088.2016.65.1.1 UR - https://m2.mtmt.hu/api/publication/3085628 ID - 3085628 N1 - Institute for Soil Science and Agricultural Chemistry, Centre of Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út 15, Budapest, 1022, Hungary Eötvös Loránd University, Faculty of Science, Institute of Geography and Earth Sciences, Budapest, Hungary Export Date: 28 January 2020 Correspondence Address: Bakacsi, Z.; Institute for Soil Science and Agricultural Chemistry, Centre of Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út 15, Hungary; email: zsofi@rissac.hu LA - Hungarian DB - MTMT ER - TY - JOUR AU - Selmeczi, Ildikó AU - Lantos, M AU - Bohn-Havas, M AU - Nagymarosy, András AU - Szego, E TI - Correlation of bio- and magnetostratigraphy of Badenian sequences from western and northern Hungary JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 63 PY - 2012 IS - 3 SP - 219 EP - 232 PG - 14 SN - 1335-0552 DO - 10.2478/v10096-012-0019-1 UR - https://m2.mtmt.hu/api/publication/2368939 ID - 2368939 N1 - Geological Institute of Hungary, Stefánia út 14, 1143 Budapest, Hungary Department of Physical and Historical Geology, Eötvös University of Sciences, Pázmány Péter Sétány 1/C, Budapest, Hungary Cited By :17 Export Date: 20 March 2024 Correspondence Address: Selmeczi, I.; Geological Institute of Hungary, Stefánia út 14, 1143 Budapest, Hungary AB - Lithological, magnetostratigraphic and paleontological (nannoplankton, foraminifers, molluscs) studies were carried out on the Badenian successions of boreholes Sopron-89, Nagylozs-1 and Sata-75 in Hungary. The correlations with the ATNTS2004 scale show that the Badenian sedimentation began during Chron C5Br thus the earliest Badenian deposits are missing in the sections. The first occurrence of Orbulina suturalis Bronnimann has been observed in Subchron C5Bn.1r, at 14.9 Ma. Although it is older than the interpolated age of 14.74 Ma in Chron C5ADr in the ATNTS2004, it is consistent with the age of 15.1 Ma obtained from recent calibration of planktonic foraminiferal bioevents. The base of the Bulimina-Bolivina Zone has been determined at 13.7 Ma in Chron C5ABr, and the Badenian/Sarmatian boundary is recorded within Chron C5AAn, at 13.15 Ma. LA - English DB - MTMT ER - TY - CONF AU - Szegő, É AU - Lantos, M AU - Bohnné, Havas M AU - Selmeczi, Ildikó AU - Nagymarosy, András ED - Pálfy, József ED - Bosnakoff, Mariann ED - Vörös, Attila TI - Kisalföldi badeni rétegsorok kapcsolata a Baden-Sooss szelvénnyel T2 - 12. Magyar Őslénytani Vándorgyűlés, Sopron, program, Előadáskivonatok, Kirándulásvezető PB - Magyarhoni Földtani Társulat PY - 2009 SP - 32 EP - 32 PG - 1 UR - https://m2.mtmt.hu/api/publication/2702176 ID - 2702176 LA - Hungarian DB - MTMT ER - TY - CHAP AU - Rasser, M W AU - Harzhauser, M AU - Anistratenko, O Y AU - Anistratenko, V V AU - Bassi, D AU - Belak, M AU - Berger, J-P AU - Bianchini, G AU - Čičić, S AU - Ćosović, V AU - Dolánková, N AU - Drobne, K AU - Filipescu, S AU - Gürs, K AU - Hladilová, Š AU - Hrvotović, H AU - Jelen, B AU - Kasiński, J R AU - Kováč, M AU - Kralj, P AU - Marjanac, T AU - Márton Péterné Szalay, Emőke AU - Mietto, P AU - Moro, A AU - Nagymarosy, András AU - Nebelsick, J H AU - Nehyba, S AU - Ogorelec, B AU - Oszczypko, N AU - Pavelić, D AU - Pavlovec, R AU - Pavšič, J AU - Petrová, P AU - Piwocki, M AU - Poljak, M AU - Pugliese, N AU - Redžepovič, R AU - Rifelj, H AU - Roetzel, R AU - Skaberne, D AU - Sliva, L AU - Stendke, G AU - Tunis, G AU - Vass, D AU - Wagreich, M AU - Wesselingh, F ED - McCann, Tom TI - Paleogene and Neogene T2 - The geology of Central Europe, Vol. 2: Mesozoic and Cenozoic PB - Geological Society of London CY - London SN - 9781862392656 PY - 2008 SP - 1031 EP - 1139 PG - 109 UR - https://m2.mtmt.hu/api/publication/1434475 ID - 1434475 LA - English DB - MTMT ER - TY - CONF AU - Bohnné, Havas M AU - Lantos, M AU - Nagymarosy, András AU - Selmeczi, Ildikó AU - Szegő, É ED - Pálfy, József ED - Bosnakoff, Mariann ED - Pazonyi, Piroska TI - Badeni képződmények korrelációja nyugat- és észak-magyarországi szelvényekben T2 - 10. Magyar Őslénytani Vándorgyűlés, Budapest, Előadáskivonatok PB - Magyarhoni Földtani Társulat C1 - Budapest PY - 2007 SP - 11 EP - 12 PG - 2 UR - https://m2.mtmt.hu/api/publication/2711737 ID - 2711737 LA - Hungarian DB - MTMT ER - TY - CHAP AU - Hably, Lilla AU - Báldi, T AU - Nagymarosy, András ED - Pálfy, József ED - Pazonyi, Piroska TI - Noszvaj, Kiseged T2 - Őslénytani kirándulások Magyarországon és Erdélyben PB - Hantken Kiadó CY - Budapest SN - 9789638743626 T3 - Geokalauz, ISSN 1789-2260 ; 1. PY - 2007 SP - 199 EP - 203 PG - 5 UR - https://m2.mtmt.hu/api/publication/1735984 ID - 1735984 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Kovac, M AU - Andreyeva-Grigorovich, A AU - Bajraktarevic, Z AU - Brzobohaty, R AU - Filipescu, S AU - Fodor, László AU - Harzhauser, M AU - Nagymarosy, András AU - Oszczypko, N AU - Pavelic, D AU - Rogl, F AU - Saftic, B AU - Sliva, L AU - Studencka, B TI - Badenian evolution of the Central Paratethys Sea: paleogeography, climate and eustatic sea-level changes JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 58 PY - 2007 IS - 6 SP - 579 EP - 606 PG - 28 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/1368433 ID - 1368433 N1 - Comenius University, Department of Geology and Paleontology, Mlynská dolina, 842 15 Bratislava, Slovakia Institute of Geological Sciences, Ukrainian National Academy of Sciences, O.Gonchar str. 55-B, Kiev, Ukraine Faculty of Science, Department of Geology and Paleontology, Horvatovac 102a, HR-10000 Zagreb, Croatia Institute of Geological Sciences, Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic Babeş-Bolyai University, Department of Geology, Str. Kogǎlniceanu 1, 400084 Cluj-Napoca, Romania Geological Institute of Hungary, Stefánia 14, H-1143 Budapest, Hungary Geological-Paleontological Department, Natural History Museum Vienna, Burgring 7, A-1014 Vienna, Austria Eötvös University, Department of Physical and Historical Geology, Pazmany Peter setany 1/C, H-1117 Budapest, Hungary Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-063 Kraków, Poland Faculty of Mining, Geology and Petroleum Engineering, Pierottijeva 6, HR-10000 Zagreb, Croatia Natural History Museum Vienna, Burgring 7, A-1014 Vienna, Austria Museum of the Earth, Polish Academy of Sciences, Al. Na Skarpie 20/26, 00-488 Warszawa, Poland Cited By :205 Export Date: 5 December 2022 Correspondence Address: Kováč, M.; Comenius University, Mlynská dolina, 842 15 Bratislava, Slovakia; email: kovacm@fns.uniba.sk AB - The Miocene Central Paratethys Sea covered wide areas of the Pannonian Basin System, bordered by the mountain chains of the Alps, Carpathians and Dinarides. The epicontinental sea spread not only in the back-arc basin area, but flooded even the Alpine-Carpathian Foredeep, situated along the front of gradually uplifting mountains. The Early Badenian (early Langhian) transgressions from the Mediterranean toward the Central Paratethys realm, via Slovenia and northern Croatia (Transtethyan Trench Corridor or Trans Dinaride Corridor) flooded the Pannonian Basin and continued along straits in the Carpathian Chain into the Carpathian Foredeep. The isolation of eastern parts of the Central Paratethys at the end of this period (late Langhian) resulted in the “Middle Badenian” salinity crisis. Thick evaporite sediments, above all halite and gypsum were deposited in the Transcarpathian Basin, Transylvanian Basin and Carpathian Foredeep. During the Late Badenian (early Serravallian), the latest full marine flooding covered the whole back-arc basin and a great part of the foredeep. The main problem is to create a model of sea connections during that time, because some authors consider the western Transtethyan Trench Corridor (Trans Dinaride Corridor) closed and there is no evidence to prove a supposed strait towards the Eastern Mediterranean. A proposed possibility is a connection towards the Konkian Sea of the Eastern Paratethys. The Badenian climate of the Central Paratethys realm can be characterized as fairly uniform, reflecting the stable subtropical conditions of the Miocene Climatic Optimum. No considerable changes in terrestrial ecosystems were documented. Nevertheless, evolution of steep landscape associated with rapid uplift of the East Alpine and Western Carpathian mountain chains (including high stratovolcanoes) caused development of vertical zonation of dry land and consequently close occurrence of different vegetation zones in a relatively small distance during this time. In the Central Paratethys Sea a slight N-S climatic gradient seems to be expressed already from the Early Badenian, but a biogeographic differentiation between basins in the North and South starts to become more prominent first during the Late Badenian, when a moderate cooling of the seawater can also be documented. The Late Badenian sea-level highstand coincides with the appearance of stress factors such as stratification of the water column and hypoxic conditions at the basin bottom in the whole area. Taking into account all bioevents and changes of paleogeography in the Central Paratethys realm, we can very roughly correlate the Early (and “Middle”) Badenian with the eustatic sea-level changes of TB 2.3, TB 2.4 or Bur5/Lan1, Lan2/Ser1 and the Late Badenian with TB 2.5 or Ser2 cycles (sensu Haq et al. 1988; Hardenbol et al. 1998). Generally, we can assign the Early Badenian transgressions to be controlled by both, tectonics (induced mainly by back-arc basin rifting) and eustacy, followed by forced regression. The Late Badenian transgression and regression were dominantly controlled by sea-level changes inside the Central Paratethys realm. LA - English DB - MTMT ER - TY - CONF AU - Kovács, Sándor AU - Brezsnyánszky, Károly AU - Buda, G AU - Haas, János AU - Szederkényi, T AU - Császár, Géza AU - Harangi, S AU - Márton Péterné Szalay, Emőke AU - Nagymarosy, András AU - Pelikán, P AU - Török, Ákos TI - Tectonostratigraphic terranes and zones juxtaposed along the Mid-Hungarianline: their contrasting evolution and relationships T2 - Proceedings of XVII. Congress of Carpathian-Balkan Geological Association PB - Vydavatelstvo Slovenskej Akadémie Vied (VEDA) C1 - Bratislava T3 - Geologica Carpathica, Special Issue Cd-Version, ISSN 1335-0552 ; 53. PY - 2002 SP - 6 EP - 6 PG - 1 UR - https://m2.mtmt.hu/api/publication/1636113 ID - 1636113 LA - English DB - MTMT ER - TY - JOUR AU - Kovács, Sándor AU - Szederkényi, T AU - Haas, János AU - Buda, György AU - Császár, Géza AU - Nagymarosy, András TI - Tectonostratigraphic terranes in the pre-Neogene basement of the Hungarian part of the Pannonian area JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 43 PY - 2000 IS - 3 SP - 225 EP - 328 PG - 104 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/152233 ID - 152233 N1 - Cited By :96 Export Date: 13 January 2023 Correspondence Address: Kovávs, S.; Geological Research Group, Muzeum krt. 4/a, Budapest, Buda H-1088, Hungary LA - English DB - MTMT ER -