Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Dan Mircea Tamas"'
Autor:
Alexandra Tamas, Dan Mircea Tamas, Gabor Tari, Csaba Krezsek, Alexandru Lapadat, Zsolt Schleder
Publikováno v:
eISSN
Many extensional basins worldwide are modified by subsequent compressional episodes, which lead to inverted structures. The structures associated with the reactivation of pre-existing faults are critically important in the formation of suitable subsu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::87cd9966133fb5182d0fbed6c88afbee
https://se.copernicus.org/articles/14/741/2023/
https://se.copernicus.org/articles/14/741/2023/
Autor:
Dan Mircea Tamas, Alexandra Tamas, Daria Dohan, Ioana Silvia Mihaela Tocariu, Zsolt Schleder, Csaba Krezsek, Janos Urai
Salt is present in many orogenic fold-and-thrust belts and it serves as an excellent décollement. This often leads to a localization of deformation (folds and thrusts) within the salt or to the development of salt diapirs. The Romanian Carpathians p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::079948b706e4e2e12aa65fc78742c36d
https://doi.org/10.5194/egusphere-egu23-5438
https://doi.org/10.5194/egusphere-egu23-5438
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:
Dan Mircea Tamas, Alexandra Tamas, Jessica Barabasch, Mark Rowan, Zsolt Schleder, Csaba Krezsek, Janos Urai
Numerous orogenic fold-and-thrust belts contain salt. It serves as an excellent décollement for folds and thrusts, and in some, diapirs had a profound influence on the structural styles. In salt-detached fold-and-thrust belts, decapitated diapirs ca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d0088ff4d99a25d424b4d631bd538bf
https://doi.org/10.5194/egusphere-egu22-4498
https://doi.org/10.5194/egusphere-egu22-4498
Autor:
Dave J. McCarthy, John R. Underhill, Ken McCaffrey, Anna Bird, David Selby, Dan Mircea Tamas, Kit Hardman, Robert E. Holdsworth, Alexandra Tamas, Eddie Dempsey
Publikováno v:
Journal of the Geological Society, 2022, Vol.179(2), pp.jgs2021-066. [Peer Reviewed Journal]
The Inner Moray Firth Basin (IMFB) forms the western arm of the North Sea trilete rift system that initiated mainly during the Late Jurassic–Early Cretaceous with the widespread development of major NE–SW-trending dip-slip growth faults. The IMFB
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d102251d941fcfa3ab6ccc8893fd40b0
https://doi.org/10.1144/jgs2021-066
https://doi.org/10.1144/jgs2021-066
Publikováno v:
International Journal of Earth Sciences. 108:1595-1614
The Carpathian Bend Zone is part of the Eastern Romanian Carpathians. The stratigraphic profile contains two levels of salt: Lower Miocene (Lower Burdigalian) and Middle Miocene (Badenian). The studied segment of the fold belt was deformed during the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::76eab81f84d25ca54ad0da7ae43828a1
https://doi.org/10.1007/s00531-019-01721-x
https://doi.org/10.1007/s00531-019-01721-x
Autor:
Dan Mircea Tamas, Istvan Szollosi, László Palcsu, Roland Szalay, Boglárka-Mercedesz Kis, Szabolcs Harangi, Andreea-Rebeka Zsigmond
The Eastern Carpathians are characterized by intense gas emissions starting from the Neogene to Quaternary volcanic structures, especially the youngest dormant volcano, Ciomadul, but occurring also far away from these, in the Cretaceous flysch units.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef184b990aa9f4fb622ebfd5a36d0631
https://doi.org/10.5194/egusphere-egu21-13506
https://doi.org/10.5194/egusphere-egu21-13506