Late Devonian–Carboniferous faulting and controlling structures and fabrics in NW Finnmark
In the SW Barents Sea, Devonian–Carboniferous collapse led to the formation of major basins and faults, e.g., the Hammerfest Basin bounded by the Troms–Finnmark Fault Complex, and rhomboid- to sigma-shaped (half-)grabens on the Finnmark Platform. High-resolution aeromagnetic and bathymetry data from...
Published in: | Norwegian Journal of Geology |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Geological Society of Norway
2019
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Subjects: | |
Online Access: | https://hdl.handle.net/10037/18392 https://doi.org/10.17850/njg99-3-5 |