The Occurrence of Chloritoid in the Hecla Hoek Formation of Prince Charles Foreland, Spitsbergen
Abstract In the Hecla Hoek rocks of Prince Charles Foreland, field evidence indicates that chloritoid has developed only where conditions of extreme stress have affected pelitic rocks of a certain type. Microscopic examination confirms that many of the chloritoid-bearing rocks are extremely strained...
Published in: | Geological Magazine |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
1956
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Online Access: | http://dx.doi.org/10.1017/s0016756800063731 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800063731 |
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crcambridgeupr:10.1017/s0016756800063731 2024-03-03T08:48:22+00:00 The Occurrence of Chloritoid in the Hecla Hoek Formation of Prince Charles Foreland, Spitsbergen Atkinson, D. J. 1956 http://dx.doi.org/10.1017/s0016756800063731 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800063731 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 93, issue 1, page 63-71 ISSN 0016-7568 1469-5081 Geology journal-article 1956 crcambridgeupr https://doi.org/10.1017/s0016756800063731 2024-02-08T08:27:57Z Abstract In the Hecla Hoek rocks of Prince Charles Foreland, field evidence indicates that chloritoid has developed only where conditions of extreme stress have affected pelitic rocks of a certain type. Microscopic examination confirms that many of the chloritoid-bearing rocks are extremely strained, and demonstrates that growth of the mineral was contemporaneous with movement. The distribution of chloritoid is in complete discordance with the pattern of regional metamorphism. Article in Journal/Newspaper Prince Charles Foreland Spitsbergen Cambridge University Press Hoek ENVELOPE(-65.050,-65.050,-66.000,-66.000) Geological Magazine 93 1 63 71 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Atkinson, D. J. The Occurrence of Chloritoid in the Hecla Hoek Formation of Prince Charles Foreland, Spitsbergen |
topic_facet |
Geology |
description |
Abstract In the Hecla Hoek rocks of Prince Charles Foreland, field evidence indicates that chloritoid has developed only where conditions of extreme stress have affected pelitic rocks of a certain type. Microscopic examination confirms that many of the chloritoid-bearing rocks are extremely strained, and demonstrates that growth of the mineral was contemporaneous with movement. The distribution of chloritoid is in complete discordance with the pattern of regional metamorphism. |
format |
Article in Journal/Newspaper |
author |
Atkinson, D. J. |
author_facet |
Atkinson, D. J. |
author_sort |
Atkinson, D. J. |
title |
The Occurrence of Chloritoid in the Hecla Hoek Formation of Prince Charles Foreland, Spitsbergen |
title_short |
The Occurrence of Chloritoid in the Hecla Hoek Formation of Prince Charles Foreland, Spitsbergen |
title_full |
The Occurrence of Chloritoid in the Hecla Hoek Formation of Prince Charles Foreland, Spitsbergen |
title_fullStr |
The Occurrence of Chloritoid in the Hecla Hoek Formation of Prince Charles Foreland, Spitsbergen |
title_full_unstemmed |
The Occurrence of Chloritoid in the Hecla Hoek Formation of Prince Charles Foreland, Spitsbergen |
title_sort |
occurrence of chloritoid in the hecla hoek formation of prince charles foreland, spitsbergen |
publisher |
Cambridge University Press (CUP) |
publishDate |
1956 |
url |
http://dx.doi.org/10.1017/s0016756800063731 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800063731 |
long_lat |
ENVELOPE(-65.050,-65.050,-66.000,-66.000) |
geographic |
Hoek |
geographic_facet |
Hoek |
genre |
Prince Charles Foreland Spitsbergen |
genre_facet |
Prince Charles Foreland Spitsbergen |
op_source |
Geological Magazine volume 93, issue 1, page 63-71 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800063731 |
container_title |
Geological Magazine |
container_volume |
93 |
container_issue |
1 |
container_start_page |
63 |
op_container_end_page |
71 |
_version_ |
1792505238471573504 |