Molluscan palaeontology of the Pliocene-Pleistocene Kap København Formation, North Greenland
The sediments of the Pliocene-Pleistocene Kap København Formation reflect a succession from isostatic conditioned regression (Member A) to transgression (Member B). Transgression rates were first slow (unit B1), then faster (unit B2), and then again slower (unit B3). The fragmented molluscan death a...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
The Commission for Scientific Research in Greenland /Danish Polar Center
1998
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Subjects: | |
Online Access: | https://tidsskrift.dk/meddrgroenland_geosci/article/view/140966 |