Geophysical characterisation of two segments of the Møre-Trøndelag Fault Complex, Mid Norway
The Møre-Trøndelag Fault Complex (MTFC) has controlled the tectonic evolution of Mid Norway and its shelf for the past 400 Myr through repeated reactivations during Palaeozoic, Mesozoic and perhaps Cenozoic times, the very last phase of reactivation involving normal to oblique-slip faulting. Despite...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2011-07-01
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| Series: | Solid Earth |
| Online Access: | http://www.solid-earth.net/2/125/2011/se-2-125-2011.pdf |