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.

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Published

1982-12-31

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.

How to Cite

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