Structural analysis of fault complexes bounding the Halten Terrace, offshore mid-Norway
The mid-Norwegian continental margin that has been tectonically active from Caledonian Orogeny to early Cenozoic time is divided into a number of structural provinces and the main tectonic phases records the transition from rifting to sea-floor spreading between Norway and Greenland in Cenozoic . Se...
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Format: | Master Thesis |
Language: | Norwegian |
Published: |
2014
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Online Access: | http://hdl.handle.net/10852/42307 http://urn.nb.no/URN:NBN:no-46686 |