A Dyke Swarm and Crustal Flexure in East Greenland
As a result of three recent expeditions to East Greenland a remarkable dyke swarm, following closely the general direction of the coast, has been found to run from the neighbourhood of Scoresby Sound to Angmagssalik, a distance of 500 miles. The dykes are dolerites of various kinds and for the most...
Published in: | Geological Magazine |
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Language: | English |
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Cambridge University Press (CUP)
1938
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Online Access: | http://dx.doi.org/10.1017/s0016756800089226 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800089226 |
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crcambridgeupr:10.1017/s0016756800089226 2024-09-15T17:39:27+00:00 A Dyke Swarm and Crustal Flexure in East Greenland Wager, L. R. Deer, W. A. 1938 http://dx.doi.org/10.1017/s0016756800089226 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800089226 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 75, issue 1, page 39-46 ISSN 0016-7568 1469-5081 journal-article 1938 crcambridgeupr https://doi.org/10.1017/s0016756800089226 2024-07-31T04:03:43Z As a result of three recent expeditions to East Greenland a remarkable dyke swarm, following closely the general direction of the coast, has been found to run from the neighbourhood of Scoresby Sound to Angmagssalik, a distance of 500 miles. The dykes are dolerites of various kinds and for the most part they are intruded into a thick Tertiary basalt series and the underlying metamorphic compled. Article in Journal/Newspaper Angmagssalik East Greenland Greenland Scoresby Sound Cambridge University Press Geological Magazine 75 1 39 46 |
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Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
As a result of three recent expeditions to East Greenland a remarkable dyke swarm, following closely the general direction of the coast, has been found to run from the neighbourhood of Scoresby Sound to Angmagssalik, a distance of 500 miles. The dykes are dolerites of various kinds and for the most part they are intruded into a thick Tertiary basalt series and the underlying metamorphic compled. |
format |
Article in Journal/Newspaper |
author |
Wager, L. R. Deer, W. A. |
spellingShingle |
Wager, L. R. Deer, W. A. A Dyke Swarm and Crustal Flexure in East Greenland |
author_facet |
Wager, L. R. Deer, W. A. |
author_sort |
Wager, L. R. |
title |
A Dyke Swarm and Crustal Flexure in East Greenland |
title_short |
A Dyke Swarm and Crustal Flexure in East Greenland |
title_full |
A Dyke Swarm and Crustal Flexure in East Greenland |
title_fullStr |
A Dyke Swarm and Crustal Flexure in East Greenland |
title_full_unstemmed |
A Dyke Swarm and Crustal Flexure in East Greenland |
title_sort |
dyke swarm and crustal flexure in east greenland |
publisher |
Cambridge University Press (CUP) |
publishDate |
1938 |
url |
http://dx.doi.org/10.1017/s0016756800089226 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800089226 |
genre |
Angmagssalik East Greenland Greenland Scoresby Sound |
genre_facet |
Angmagssalik East Greenland Greenland Scoresby Sound |
op_source |
Geological Magazine volume 75, issue 1, page 39-46 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800089226 |
container_title |
Geological Magazine |
container_volume |
75 |
container_issue |
1 |
container_start_page |
39 |
op_container_end_page |
46 |
_version_ |
1810479974970294272 |