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Post-Caledonian brittle faults along the SW Barents Sea Margin

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Academic year: 2022

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important to settle if they represent distinct tectonic events, a progressive evolution by exhumation of the margin, or alternatively, both, with a progressive re-use of hyperextended SW Barents Sea margin: New insights into onshore and offshore margin architecture (8) As the studied fault zones are the onshore portions of large fault complexes that continue offshore, it is likely that the studied fault zones are analogous to basement-seated faults institutions. We would also like to thank the Norwegian Mapping Authority and the Norwegian Armed Forces for sharing and allowing us to publish illustrations of the

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