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...

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Bibliographic Details
Main Authors: Símonarson, Leifur A., Petersen, Kaj Strand, Funder, Svend
Format: Article in Journal/Newspaper
Language:English
Published: The Commission for Scientific Research in Greenland /Danish Polar Center 1998
Subjects:
Kap
Online Access:https://tidsskrift.dk/meddrgroenland_geosci/article/view/140966