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

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...

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Published in:Geological Magazine
Main Authors: Gobbett, D. J., Wilson, C. B.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1960
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800061835
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800061835
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spelling crcambridgeupr:10.1017/s0016756800061835 2024-06-23T07:53:16+00:00 The Oslobreen Series, Upper Hecla Hoek of Ny Friesland, Spitsbergen Gobbett, D. J. Wilson, C. B. 1960 http://dx.doi.org/10.1017/s0016756800061835 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800061835 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 97, issue 6, page 441-457 ISSN 0016-7568 1469-5081 journal-article 1960 crcambridgeupr https://doi.org/10.1017/s0016756800061835 2024-06-12T04:04:42Z 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. Article in Journal/Newspaper Greenland Ny Friesland Spitsbergen Cambridge University Press Greenland Hoek ENVELOPE(-65.050,-65.050,-66.000,-66.000) Ny Friesland ENVELOPE(16.847,16.847,79.498,79.498) Geological Magazine 97 6 441 457
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collection Cambridge University Press
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language English
description 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.
format Article in Journal/Newspaper
author Gobbett, D. J.
Wilson, C. B.
spellingShingle Gobbett, D. J.
Wilson, C. B.
The Oslobreen Series, Upper Hecla Hoek of Ny Friesland, Spitsbergen
author_facet Gobbett, D. J.
Wilson, C. B.
author_sort Gobbett, D. J.
title The Oslobreen Series, Upper Hecla Hoek of Ny Friesland, Spitsbergen
title_short The Oslobreen Series, Upper Hecla Hoek of Ny Friesland, Spitsbergen
title_full The Oslobreen Series, Upper Hecla Hoek of Ny Friesland, Spitsbergen
title_fullStr The Oslobreen Series, Upper Hecla Hoek of Ny Friesland, Spitsbergen
title_full_unstemmed The Oslobreen Series, Upper Hecla Hoek of Ny Friesland, Spitsbergen
title_sort oslobreen series, upper hecla hoek of ny friesland, spitsbergen
publisher Cambridge University Press (CUP)
publishDate 1960
url http://dx.doi.org/10.1017/s0016756800061835
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800061835
long_lat ENVELOPE(-65.050,-65.050,-66.000,-66.000)
ENVELOPE(16.847,16.847,79.498,79.498)
geographic Greenland
Hoek
Ny Friesland
geographic_facet Greenland
Hoek
Ny Friesland
genre Greenland
Ny Friesland
Spitsbergen
genre_facet Greenland
Ny Friesland
Spitsbergen
op_source Geological Magazine
volume 97, issue 6, page 441-457
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800061835
container_title Geological Magazine
container_volume 97
container_issue 6
container_start_page 441
op_container_end_page 457
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