Biostratigraphic reconnaissance in the Lower Palaeozoic of western North Greenland

Authors

  • P.R Dawes
  • J.S Peel

DOI:

https://doi.org/10.34194/rapggu.v121.7872

Abstract

Sections and fossil collections resulting from activities under Operation Grant Land 1965-66 in the Hall Land - Wulff Land region of western North Greenland are briefly discussed. Strongly tectonised Lower Cambrian to Silurian strata are present in the northern part of the area in association with the Wulff Land anticline and the Nyeboe Land fault zone. To the south, platform and deep-water trough sequences are generally little disturbed and strata range in age from Middle Ordovician to Late Silurian (Pridoli). Most stratigraphic units can be accommodated in stratigraphic schemes established in Washington Land, to the west, or Peary Land, to the east.

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Published

1984-12-31

How to Cite

Dawes, P., & Peel, J. (1984). Biostratigraphic reconnaissance in the Lower Palaeozoic of western North Greenland. Rapport Grønlands Geologiske Undersøgelse, 121, 19–51. https://doi.org/10.34194/rapggu.v121.7872