An erosional structure in a layered dolerite dyke, West Greenland

Summary A vertical channel structure within a layered dolerite dyke resulted from differential magmatic flow. Layering in both dyke and channel is formed of more feldspathic dolerite attributed to fluctuations in water vapour pressure and supercooling during crystallization.

Bibliographic Details
Published in:Geological Magazine
Main Author: Williams, H. R.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1976
Subjects:
Geology
Greenland
Online Access:http://dx.doi.org/10.1017/s001675680004303x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680004303X
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spelling crcambridgeupr:10.1017/s001675680004303x 2024-03-03T08:44:56+00:00 An erosional structure in a layered dolerite dyke, West Greenland Williams, H. R. 1976 http://dx.doi.org/10.1017/s001675680004303x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680004303X en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 113, issue 1, page 77-82 ISSN 0016-7568 1469-5081 Geology journal-article 1976 crcambridgeupr https://doi.org/10.1017/s001675680004303x 2024-02-08T08:28:45Z Summary A vertical channel structure within a layered dolerite dyke resulted from differential magmatic flow. Layering in both dyke and channel is formed of more feldspathic dolerite attributed to fluctuations in water vapour pressure and supercooling during crystallization. Article in Journal/Newspaper Greenland Cambridge University Press Greenland Geological Magazine 113 1 77 82
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
spellingShingle Geology
Williams, H. R.
An erosional structure in a layered dolerite dyke, West Greenland
topic_facet Geology
description Summary A vertical channel structure within a layered dolerite dyke resulted from differential magmatic flow. Layering in both dyke and channel is formed of more feldspathic dolerite attributed to fluctuations in water vapour pressure and supercooling during crystallization.
format Article in Journal/Newspaper
author Williams, H. R.
author_facet Williams, H. R.
author_sort Williams, H. R.
title An erosional structure in a layered dolerite dyke, West Greenland
title_short An erosional structure in a layered dolerite dyke, West Greenland
title_full An erosional structure in a layered dolerite dyke, West Greenland
title_fullStr An erosional structure in a layered dolerite dyke, West Greenland
title_full_unstemmed An erosional structure in a layered dolerite dyke, West Greenland
title_sort erosional structure in a layered dolerite dyke, west greenland
publisher Cambridge University Press (CUP)
publishDate 1976
url http://dx.doi.org/10.1017/s001675680004303x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680004303X
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_source Geological Magazine
volume 113, issue 1, page 77-82
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s001675680004303x
container_title Geological Magazine
container_volume 113
container_issue 1
container_start_page 77
op_container_end_page 82
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