Continent-ocean-transition across a trans-tensional margin segment: off Bear Island, Barents Sea

P>A 410 km long Ocean Bottom Seismometer profile spanning from the Bear Island, Barents Sea to oceanic crust formed along the Mohns Ridge has been modelled by use of ray-tracing with regard to observed P-waves. The northeastern part of the model represents typical continental crust, thinned from...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Czuba, Wojciech, Grad, Marek, Mjelde, Rolf, Guterch, Aleksander, Libak, Audun, Krüger, Frank (Prof. Dr.), Murai, Yoshio, Schweitzer, Johannes
Format: Article in Journal/Newspaper
Language:English
Published: 2011
Subjects:
Online Access:https://publishup.uni-potsdam.de/frontdoor/index/index/docId/37051
https://doi.org/10.1111/j.1365-246X.2010.04873.x