2024
DOI: 10.1111/bre.12904
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Multi‐mode gravity tectonics during northern North Sea rifting: the Snorre fault block case

Haakon Fossen

Abstract: Continental rifts are characterized by up to 30 km wide rotated fault blocks with stratigraphic dip away from the central rift axis. Although gravity‐induced mass movements are well known features of collapsed fault block crests, I here demonstrate the occurrence of polymodal gravity‐driven mass transport down the back slope of a first‐order rift fault block. I identify (1) early sliding related to syntectonic crestal collapse of second‐order rift faults, (2) large‐scale bed‐parallel sliding of the L‐M Jurassi… Show more

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