Southwest Barents Sea rift basin evolution: comparing results from backstripping and time-forward modelling-Reference-Cited by-同舟云学术

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Southwest Barents Sea rift basin evolution: comparing results from backstripping and time-forward modelling

Published:2013-10-03 Issue:4 Volume:26 Page:550-566
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Res

Author:

Clark S. A.¹,Glorstad-Clark E.¹,Faleide J. I.¹,Schmid D.²³,Hartz E. H.²⁴,Fjeldskaar W.⁵⁶

Affiliation:

1. Department of Geosciences; University of Oslo; Oslo Norway

2. Physics of Geological Processes; University of Oslo; Oslo Norway

3. GeoModelling Solutions; Zürich Switzerland

4. Det norske oljeselskap; Trondheim Norway

5. TECTONOR AS; Stavanger Norway

6. Department of Petroleum Engineering; University of Stavanger; Stavanger Norway

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/bre.12039/fullpdf

Reference64 articles.

1. Offshore prolongation of Caledonian structures and basement characterisation in the western Barents Sea from geophysical modelling;Barrère;Tectonophysics,2009

2. A physical explanation of the relation between flank uplifts and the breakup unconformity at rifted continental margins;Braun;Geology,1989

3. Ottar-Basin, SW Barents-Sea - a major Upper Paleozoic rift basin containing large volumes of deeply buried salt;Breivik;Basin Res.,1995

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