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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Bibliographic Details
Main Author: Weldemicael, Issak Habtemicael
Format: Master Thesis
Language:Norwegian
Published: 2014
Subjects:
Kya
Online Access:http://hdl.handle.net/10852/42307
http://urn.nb.no/URN:NBN:no-46686