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Modelling of OBS Data Across the Vestbakken Volcanic Province

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dc.contributor.author Sørensen, Asude Arslan
dc.date.accessioned 2011-10-20T08:13:03Z
dc.date.available 2011-10-20T08:13:03Z
dc.date.issued 2011
dc.date.submitted 2011-05-31 en_US
dc.identifier.uri http://hdl.handle.net/1956/5112
dc.description.abstract A P-Wave model of a 384 km long Ocean Bottom Seismometer profile has been modelled by use of ray-tracing. The profile, Bear Island South (BIS-2008), crossses the transtensional Vestbakken Volcanic Province and the boundary between northern Atlantic oceanic crust of the Barents Sea continental platform. This study is a part of the 4th International Polar Year (IPY) international project entitled The Dynamic Continental Margin Between the Mid-Atlantic-Ridge (Mohns Ridge, Knipovich Ridge) and the Bear Island Region'. The thickness of crust varies greatly along the profile, from 7 km at the oceanic part (southwest) to approximately 32 km at the continental part (northeast). Northeastern part of the profile represents continental crust and southwestern part shows the oceanic crust. The transition from oceanic crust to continental crust occurs in a narrow zone of 30 km width. The continent ocean boundary (COB) is located in the range 190-220 km along the profile. The Hornsund and Knølegga fault zones are modelles as significant lateral variations in velocity. en
dc.format.extent 6110235 bytes en_US
dc.format.mimetype application/pdf en_US
dc.language.iso eng en
dc.publisher The University of Bergen en
dc.rights Copyright the author. All rights reserved. en
dc.subject OBS en
dc.subject Modeling en
dc.subject Vestbakken en
dc.title Modelling of OBS Data Across the Vestbakken Volcanic Province en
dc.type Master thesis en
dc.type.degree Master i Geovitenskap en_US
dc.type.course GEOV399 en_US
dc.subject.nsi VDP::Mathematics and natural science: 400::Geosciences: 450 en
dc.subject.archivecode Mastergrad en_US
dc.subject.nus 756199 en_US
dc.type.program MAMN-GEOV en_US


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