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...
Published in: | Journal of the Geological Society |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Geological Society of London
2023
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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 |