Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Edit Babinszki"'
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 285:303-312
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::10dc67aa92daa5bf196de6301fa18da2
https://doi.org/10.1127/njgpa/2017/0682
https://doi.org/10.1127/njgpa/2017/0682
Autor:
Sampat K. Tandon, Annamária Nádor, Zsófia Medzihradszky, Rajiv Sinha, Ashish Kumar Singh, Edit Thamó-Bozsó, Edit Babinszki, Árpád Magyari, Zoltán Unger
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 299:1-14
Four drill cores and a clay pit section have been examined in the southern part of the Koros plain to understand the history and controls on alluvial sedimentation for the last ~ 40 ka. Four facies groups were identified, such as channel, channel mar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::109205bae64f73ef8fbadba6e042b94a
https://doi.org/10.1016/j.palaeo.2010.09.018
https://doi.org/10.1016/j.palaeo.2010.09.018
Publikováno v:
Sedimentary Geology. 202:174-192
Fine-grained sandy–silty channel–belt and floodplain deposits of the Berettyo–Koros Rivers, a main eastern transverse tributary system of the modern Tisza River in the eastern part of the Pannonian Basin, were deposited during the Late Pleistoc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2eebb1b59d2b64c9d325f2687d9b0a60
https://doi.org/10.1016/j.sedgeo.2007.03.001
https://doi.org/10.1016/j.sedgeo.2007.03.001
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 252:626-636
Lake Pannon was a large lake at the southern margin of the European plate, which separated from the Central Paratethys at the Sarmatian–Pannonian boundary and was filled completely with sediment during the Pliocene. The separation produced an endem
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::23088c8dcec2d2ac29ffb6aff795b40e
https://doi.org/10.1016/j.palaeo.2007.06.001
https://doi.org/10.1016/j.palaeo.2007.06.001
Publikováno v:
Facies. 52:209-220
Oxygen availability is considered to have been a major factor in shaping the sedimentary facies and biofacies of a Late Miocene (8–8.5 Ma old) Lake Pannon sequence studied in the Kozma-street outcrop in Budapest-Kobanya. The sequence contains blue
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32331814149f7b1b9b9a464307c7dbd7
https://doi.org/10.1007/s10347-005-0036-y
https://doi.org/10.1007/s10347-005-0036-y
Publikováno v:
Geologos. 16
The Upper Permian Boda Claystone Formation (BCF) in SW Hungary has been previously been identified as a saline lake deposit. A country-wide screening found this 800–1000 m thick succession the most suitable for the disposal of high-level radioactiv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b4a498015ff1e5610f52766c138414a4
https://doi.org/10.2478/v10118-010-0002-1
https://doi.org/10.2478/v10118-010-0002-1
Autor:
Radovan Pipík, Miklós Lantos, Imre Magyar, Stjepan Ćorić, István Cziczer, Edit Babinszki, Mária Sütő-Szentai, Pál Müller, Koraljka Bakrač, Madelaine Böhme
Life and depositional environments in the sub- littoral 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 coe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d46d8b7999c4829bd17119265111e38
https://www.bib.irb.hr/379059
https://www.bib.irb.hr/379059
Publikováno v:
Thamó-Bozsó, E, Murray, A S, Nádor, A, Magyari, Á & Babinszki, E 2007, ' Investigation of river network evolution using luminescence dating and heavy mineral analysis of Late-Quaternary fluvial sands from the Great Hungarian Plain ', Quaternary Geochronology, vol. 2, pp. 168-173 .
Aarhus University
Aarhus University
To reconstruct the evolution of Late-Quaternary river network in the southeastern part of the Great Hungarian Plain, we have used optically stimulated luminescence (OSL) and heavy mineral analysis of 25 sand samples from the upper 2–8 m of the fluv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::647b81e3fbe98470630666574f9fdd47
https://pure.au.dk/portal/da/publications/investigation-of-river-network-evolution-using-luminescence-dating-and-heavy-mineral-analysis-of-latequaternary-fluvial-sands-from-the-great-hungarian-plain(9a3baf60-fbfe-11dc-b919-000ea68e967b).html
https://pure.au.dk/portal/da/publications/investigation-of-river-network-evolution-using-luminescence-dating-and-heavy-mineral-analysis-of-latequaternary-fluvial-sands-from-the-great-hungarian-plain(9a3baf60-fbfe-11dc-b919-000ea68e967b).html