Recurrent mass-wasting in the Sørvestsnaget Basin Southwestern Barents Sea: A test of multiple hypotheses
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文摘

The Sørvestsnaget Basin is characterized by alternating cycles of sea level fall and rise.

Mass-transport deposits (MTDs) in the area occur from Miocene to Pleistocene time.

The MTDs include heterogeneous and homogeneous types.

Older MTDs are related to non-glacial subaqueous erosion.

The younger MTDs are connected to large-scale glaciation that affected the study area.

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