Devonian–Carboniferous extension and Eurekan inversion along an inherited WNW–ESE-striking fault system in Billefjorden, Svalbard

Background The Billefjorden area in central Spitsbergen hosts thick Lower–lowermost Upper Devonian, late–post-Caledonian collapse deposits presumably deformed during the Late Devonian Svalbardian Orogeny. These rocks are juxtaposed against Proterozoic basement rocks along the Billefjorden Fault Zone...

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Bibliographic Details
Main Authors: Koehl, Jean-Baptiste P., Allaart, Lis, Noormets, Riko
Format: Text
Language:English
Published: F1000 Research Limited
Subjects:
Online Access:https://doi.org/10.12688/openreseurope.15936.2