Conodonts from the Ordovician of East Greenland

Authors

  • M.P Smith

DOI:

https://doi.org/10.34194/rapggu.v108.7777

Abstract

The Cambro-Ordovician of East Greenland outcrops in a narrow belt between Canning Land (71°36') and C. H. Ostenfeld Nunatak (72°22'N). The uppermost three units, namely the Cape Weber, Narwhale Sound and Heim Bjerge Formations of the 4000 m thick sequence, have been sampled for conodonts.

Cover image for volume 108

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Published

1982-12-31

How to Cite

Smith, M. (1982). Conodonts from the Ordovician of East Greenland. Rapport Grønlands Geologiske Undersøgelse, 108, 14–14. https://doi.org/10.34194/rapggu.v108.7777

Issue

Vol. 108 (1982): Palaeontology of Greenland: short contributions

Section

Article

License

This article is distributed under a CC-BY 4.0 licence, permitting free redistribution and reproduction for any purpose, even commercial, provided proper citation of the original work. Author(s) retain copyright over the article contents.