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...

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Published in:Geological Magazine
Main Author: Atkinson, D. J.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1956
Subjects:
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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spelling 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
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