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

• Published in: Geophysical Journal International
• Main Authors: Czuba, W., Grad, M., Mjelde, R., Guterch, A., Libak, A., Krüger, F., Murai, Y., Schweitzer, J., Schmidt-Aursch, Mechita C., Faleide, J. I.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2011
• Subjects: Barents Sea; Bear Island; Hornsund; Knipovich Ridge; Vestbakken
• Online Access: https://epic.awi.de/id/eprint/25700/; https://doi.org/10.1111/j.1365-246X.2010.04873.x; https://hdl.handle.net/10013/epic.38700

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 ca. 3...