The Distinction between Chlorophaeite and Palagonite

In a recent paper, Dr. L. L. Fermor (12) discusses the composition of chlorophaeite and palagonite and the employment of these terms, with special reference to the present writer's view of this subject, reached principally through a study of the palagonitetuffs of Iceland (11). In an earlier ex...

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Published in:Geological Magazine
Main Author: Peacock, Martin A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1930
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800099155
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800099155
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spelling crcambridgeupr:10.1017/s0016756800099155 2024-04-28T08:25:47+00:00 The Distinction between Chlorophaeite and Palagonite Peacock, Martin A. 1930 http://dx.doi.org/10.1017/s0016756800099155 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800099155 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 67, issue 4, page 170-178 ISSN 0016-7568 1469-5081 Geology journal-article 1930 crcambridgeupr https://doi.org/10.1017/s0016756800099155 2024-04-02T06:55:28Z In a recent paper, Dr. L. L. Fermor (12) discusses the composition of chlorophaeite and palagonite and the employment of these terms, with special reference to the present writer's view of this subject, reached principally through a study of the palagonitetuffs of Iceland (11). In an earlier extended study of Indian traps Dr. Fermor had concluded that the orange and brown chlorophaeite-like bodies, often called “palagonite” by the Indian Survey petrographers, are identical with chlorophaeite, and that the similar associated greenish substance, also embraced in the term “palagonite” by these workers, is perhaps, when anisotropic, the chlorite delessite (10, p. 133). One inference from these observations is that palagonite comprises chlorophaeite and the associated green substance; another is that the application of palagonite to these bodies was primarily a misnomer. Article in Journal/Newspaper Iceland Cambridge University Press Geological Magazine 67 4 170 178
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
spellingShingle Geology
Peacock, Martin A.
The Distinction between Chlorophaeite and Palagonite
topic_facet Geology
description In a recent paper, Dr. L. L. Fermor (12) discusses the composition of chlorophaeite and palagonite and the employment of these terms, with special reference to the present writer's view of this subject, reached principally through a study of the palagonitetuffs of Iceland (11). In an earlier extended study of Indian traps Dr. Fermor had concluded that the orange and brown chlorophaeite-like bodies, often called “palagonite” by the Indian Survey petrographers, are identical with chlorophaeite, and that the similar associated greenish substance, also embraced in the term “palagonite” by these workers, is perhaps, when anisotropic, the chlorite delessite (10, p. 133). One inference from these observations is that palagonite comprises chlorophaeite and the associated green substance; another is that the application of palagonite to these bodies was primarily a misnomer.
format Article in Journal/Newspaper
author Peacock, Martin A.
author_facet Peacock, Martin A.
author_sort Peacock, Martin A.
title The Distinction between Chlorophaeite and Palagonite
title_short The Distinction between Chlorophaeite and Palagonite
title_full The Distinction between Chlorophaeite and Palagonite
title_fullStr The Distinction between Chlorophaeite and Palagonite
title_full_unstemmed The Distinction between Chlorophaeite and Palagonite
title_sort distinction between chlorophaeite and palagonite
publisher Cambridge University Press (CUP)
publishDate 1930
url http://dx.doi.org/10.1017/s0016756800099155
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800099155
genre Iceland
genre_facet Iceland
op_source Geological Magazine
volume 67, issue 4, page 170-178
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800099155
container_title Geological Magazine
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container_issue 4
container_start_page 170
op_container_end_page 178
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