Zobrazeno 41 - 50
of 180
pro vyhledávání: '"Ustaszewski, Kamil"'
Publikováno v:
International Journal of Earth Sciences. Jan2015, Vol. 104 Issue 1, p1-26. 26p.
The southern end of the Upper Rhine Graben (URG) is formed by a major continental transfer zone, which was localised by the reactivation of ENE-oriented basement faults of Late Palaeozoic origin. A combination of subcrop data (derived from exploratio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______805::4d7350d3f9f9aac249d088123b6f82c3
http://doc.rero.ch/record/314130/files/531_2004_Article_454.pdf
http://doc.rero.ch/record/314130/files/531_2004_Article_454.pdf
Autor:
Ustaszewski, Kamil, Schmid, Stefan
The southernmost Upper Rhine Graben and adjacent Jura experienced basement-rooted shortening that occurred after the deposition of the Pliocene fluvial "Sundgau gravels”. Folds affecting the base of these gravels systematically trend NE to ENE. Com
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______805::661ce6a307d61a9b33d56bd47b42fc07
http://doc.rero.ch/record/314407/files/15_2007_Article_1226.pdf
http://doc.rero.ch/record/314407/files/15_2007_Article_1226.pdf
The long-lasting convergence between the European and Adriatic plate led to the formation of the Dinar- ides fold and thrust belt. The Cretaceous deformation of the Internal Dinarides, composed by ophiolite-bar- ing nappes, is older than the mid Eoce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::845f4cae30e835fa6eea0b2898ad48e7
https://www.bib.irb.hr/956482
https://www.bib.irb.hr/956482
Autor:
Tomljenović, Bruno, Balling, Philipp, Matoš, Bojan, Vlahović, Igor, Schmid, Stefan, Ustaszewski, Kamil, Blažok, Lovro, Posarić, Dino, Širol, Andre
Mt. Velebit is the most prominent geomorphological structure in the central part of the External Dinarides fold-thrust belt formed by contraction along the eastern margin of the Adriatic plate during Cenozoic convergence between the Adriatic and Euro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::7bf389f15a5e7695cf237ecdb7415535
https://www.bib.irb.hr/956473
https://www.bib.irb.hr/956473
Publikováno v:
Geologija (0016-7789); 2021, Vol. 64 Issue 1, p21-33, 13p
Autor:
Le Breton, Eline, Brune, Sascha, Ustaszewski, Kamil, Zahirovic, Sabin, Seton, Maria, Müller, R. Dietmar
Publikováno v:
Solid Earth Discussions; 10/8/2020, p1-42, 42p
Autor:
Tomljenović, Bruno, Balling, Phillip, Matoš, Bojan, Vlahović, Igor, Herak, Marijan, Herak, Davorka, Blažok, Lovro, Posarić, Dino, Širol, Andre, Schmid, Stefan, Ustaszewski, Kamil
Mt. Velebit lies in the central part of external Dinarides formed by thrusting along the eastern margin of the Adriatic plate during Cenozoic convergence between the Adriatic and European plates. At present, the Adria–Europe convergence between Adr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::cd982b535252ec6c7fe0c5373402d9ce
https://www.bib.irb.hr/907081
https://www.bib.irb.hr/907081