Zobrazeno 1 - 10
of 200
pro vyhledávání: '"Flueh, Ernst R"'
Publikováno v:
In Tectonophysics 5 February 2020 776
Autor:
Jintasaeranee, Pachoenchoke, Weinrebe, Wilhelm, Klaucke, Ingo, Snidvongs, Anond, Flueh, Ernst R.
Publikováno v:
In Journal of Asian Earth Sciences 2 March 2012 46:78-85
Publikováno v:
In Sedimentary Geology 2007 196(1):269-277
Autor:
Michaud, François, Chabert, Anne, Collot, Jean-Yves, Sallarès, Valentí, Flueh, Ernst R., Charvis, Philippe, Graindorge, David, Gustcher, Marc-André, Bialas, Joerg
Publikováno v:
In Marine Geology 2005 216(4):205-219
Autor:
Aarseth, Iselin, Mjelde, Rolf, Breivik, Asbjørn Johan, Minakov, Alexander, Faleide, Jan Inge, Flueh, Ernst R., Huismans, Ritske
Publikováno v:
Aarseth, Iselin Mjelde, Rolf Breivik, Asbjørn Johan Minakov, Alexander Faleide, Jan Inge Flueh, Ernst R. Huismans, Ritske . Crustal structure and evolution of the Arctic Caledonides: Results fromcontrolled-source seismology. Tectonophysics. 2017, 718, 9-24
Tectonophysics
Tectonophysics
Externí odkaz:
http://hdl.handle.net/10852/60731
https://www.duo.uio.no/bitstream/handle/10852/60731/2/Aarseth_Tectonophysics_2017_postprint.pdf
https://www.duo.uio.no/bitstream/handle/10852/60731/2/Aarseth_Tectonophysics_2017_postprint.pdf
Publikováno v:
Breivik, Asbjørn Johan Faleide, Jan Inge Mjelde, Rolf Flueh, Ernst R. Murai, Yoshio . A new tectono-magmatic model for the Lofoten/Vesterålen Margin at the outer limit of the Iceland Plume influence. Tectonophysics. 2017, 718, 25-44
Tectonophysics
Tectonophysics
Publikováno v:
In Tectonophysics 2001 341(1):179-193
Autor:
Kukowski, Nina *, Schillhorn, Thies, Huhn, Katrin, von Rad, Ulrich, Husen, Stephan, Flueh, Ernst R.
Publikováno v:
In Marine Geology 2001 173(1):1-19
Autor:
Kvarven, Trond, Ebbing, Jorg, Mjelde, Rolf, Faleide, Jan Inge, Libak, Audun, Thybo, Hans, Flueh, Ernst R., Murai, Yoshio
Publikováno v:
Tectonophysics. 626:21-40
The More Margin in the NE Atlantic represents a dominantly passive margin with an unusual abrupt transition from alpine morphology onshore to a deep sedimentary basin offshore. In order to study this transition in detail, three ocean bottom seismomet
Autor:
Starostenko, V., Janik, T., Stephenson, R., Gryn, D., Rusakov, O., Czuba, W., Sroda, P., Grad, M., Guterch, A., Flueh, Ernst R., Thybo, H., Artemieva, I., Tolkunov, A., Sydorenko, G., Lysynchuk, D., Omelchenko, V., Kolomiyets, K., Legostaeva, O., Dannowski, Anke, Shulgin, Alexey
Publikováno v:
Tectonic Evolution of the Eastern Black Sea and Caucasus., ed. by Sosson, M., Stephenson, R. A. and Adamia, S. A. Special Publications Geological Society London, 428 . GSL (Geological Society London), London, pp. 199-220.
The DOBRE-2 wide-angle reflection and refraction profile was acquired in June 2007 as a direct, southwestwards prolongation of the 1999 DOBREfraction’99 that crossed the Donbas Foldbelt in eastern Ukraine. It crosses the Azov Massif of the East Eur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2386::a62ee8a6934dcfc56b36a6f1847db797
http://oceanrep.geomar.de/31288/
http://oceanrep.geomar.de/31288/