Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Csaba Krézsek"'
Autor:
Alexandra Tamas, Dan Mircea Tamas, Bianca Copot, Ioana Silvia Mihaela Tocariu, Daria Dohan, Zsolt Schléder, Csaba Krézsek
Fold and thrust belts are a notoriously challenging environment when it comes to providing structural models for the subsurface, and the Romanian Carpathians are no exception. Hosting the largest onshore oil fields in Romania, this is a highly mature
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ac30a6b6576311ed4cadf887013160f
https://doi.org/10.5194/egusphere-egu23-6425
https://doi.org/10.5194/egusphere-egu23-6425
Autor:
Rattanaporn Fongngern, Thomas Hess, Cornel Olariu, Csaba Krézsek, Ronald J. Steel, David Mohrig
Publikováno v:
Sedimentology. 65:1447-1481
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f59f5ee7226c714f9a2ff35a4533a95f
https://doi.org/10.1111/sed.12430
https://doi.org/10.1111/sed.12430
Publikováno v:
Terra Nova. 30:63-71
Before reaching the Black Sea, the Danube River passes through a string of Para-Tethyan (Vienna, Pannonian and Western and Eastern Dacian) basins. The key question is, when and how did the Danube River became a continental-scale river with a drainage
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3edc46a1bbf69aa0b158c2c50e7f8240
https://doi.org/10.1111/ter.12308
https://doi.org/10.1111/ter.12308
Autor:
Cornel Olariu, Csaba Krézsek
Publikováno v:
Global and Planetary Change. 197:103391
Large rivers typically form in the final phase of evolution of sedimentary basins. By that time the sediment supply balances out the accommodation, local rivers coalesce into larger rivers and seek pathways to flow out of the basin into areas where a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::941f4a70619006131f94b9c2fc1126b2
https://doi.org/10.1016/j.gloplacha.2020.103391
https://doi.org/10.1016/j.gloplacha.2020.103391
Publikováno v:
Basin Research. 28:770-795
Late Miocene lacustrine clinoforms of up to 400 m high are mapped using a 1700 km2 3-D seismic data set in the Dacian foreland basin, Romania. Eight Meotian clinoforms, constructed by sediment from the South Carpathians, prograded around 25 km toward
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c4d87922690fed58b53759a51297f153
https://doi.org/10.1111/bre.12132
https://doi.org/10.1111/bre.12132
Autor:
Paul Andriessen, Sandra Merten, Liviu Matenco, Stefan M. Schmid, Sierd Cloetingh, Csaba Krézsek
Publikováno v:
Terra Nova. 22:155-165
Sequence stratigraphy in the hinterland, kinematic analysis of thin-skinned thrusting in the foreland and thermochronological tracking of exhumation in the orogenic core are combined to quantify the mechanics of an orogen with low topographic build-u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9f732fc9d9bef919e8b5c4b7c02d9938
https://doi.org/10.1111/j.1365-3121.2010.00931.x
https://doi.org/10.1111/j.1365-3121.2010.00931.x
Publikováno v:
Krezsek, C, Filipescu, S, Silye, L, Matenco, L C & Doust, H 2010, ' Miocene facies associations and sedimentary evolution of the Southern Transylvanian Basin (Romania): implications for hydrocarbon exploration ', Marine and Petroleum Geology, vol. 27, pp. 191-214 . https://doi.org/10.1016/j.marpetgeo.2009.07.009
Marine and Petroleum Geology, 27, 191-214. Elsevier BV
Marine and Petroleum Geology, 27, 191-214. Elsevier BV
The Transylvanian Basin is a mature hydrocarbon province of Romania characterized by two petroleum systems: Mesozoic (thermogenic) and Miocene (biogenic). An extensive outcrop-based sedimentological and micropaleontological study correlated to seismi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b7aa0eb2da447c9f8903d2ba0f04d956
https://hdl.handle.net/1871/29434
https://hdl.handle.net/1871/29434