Structural evolution of the reactivated Møre–Trøndelag Fault Complex, Fosen Peninsula, Norway

The ENE–WSW-trending Møre–Trøndelag Fault Complex (MTFC) in Central Norway is a 10–50 km-wide, steeply dipping reactivated fault zone. Onshore, it transects Devonian sedimentary rocks and a series of east to SE transported metamorphic nappes, which were emplaced during the Scandian (Silurian–Devonia...

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Bibliographic Details
Published in:Journal of the Geological Society
Main Authors: Watts, Lee M., Holdsworth, Robert E., Roberts, David, Sleight, Janine M., Walker, Richard J.
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of London 2023
Subjects:
Online Access:http://dro.dur.ac.uk/38420/
http://dro.dur.ac.uk/38420/1/38420.pdf
https://doi.org/10.1144/jgs2022-139