The oslobreen series, upper Hecla Hoek of Ny Friesland, Spitsbergen
By: Gobbett, D.J.
Contributor(s): Wilson, C.B.
Material type: ArticleDescription: 441-457p ; Illustration.Subject(s): Oslobreen series - Hecla hoek - Ny Friesland - Spitsbergen | Limestone - Oslobreen - Spitsbergen | Paleozoic | Historical geology - Arctic region In: Geological magazine : Vol 97 Iss. 1-6 Year. 1960Summary: Abstract Six 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.Item type | Current location | Collection | Call number | Status | Date due | Barcode |
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Article | Library and Information Centre Periodical Section | Bound Journal Collection | Not for loan | 002545_70 | ||
Serials/Scientific Journal | Library and Information Centre Periodical Section | Bound Journal Collection | 550 GEO (Browse shelf) | Damaged | 002545 |
Abstract
Six 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.
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