The Oslobreen Series, Upper Hecla Hoek of Ny Friesland, Spitsbergen

Author:

Gobbett D. J.,Wilson C. B.

Abstract

AbstractSix formations, totalling 1,210 metres and grouped as the Oslobreen Series, are dominantly of dolomite and limestone often with evidence of discontinuous deposition. They contain a Lower Cambrian and a Canadian fauna. The succession is similar to those of this age in N.W. Scotland, where a revised thickness is given, and in E. Greenland. A new species of Canadian trilobite (Hystricurus) is described in the Appendix.

Publisher

Cambridge University Press (CUP)

Subject

Geology

Reference17 articles.

1. The geology of the Cambro-Ordovician rocks of central East Greenland;Cowie;Medd. Grønland,1957

2. Stratigraphy of the Garden City Formation in north-eastern Utah and its trilobite faunas;Ross;Bull. Peabody Mus.,1951

3. The Caledonian sequence in Ny Friesland, Spitsbergen;Harland;Quart. J. geol. Soc. Lond.,1959

4. Report on the geological investigations of the Hornsund area;Birkenmajer;Bull. Acad. Sci. Polonaise. Ser. sci. chim. geol. geogr.,1959

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