The Geology of North-East Jan Mayen
Abstract Field observations collected on a short expedition to Jan Mayen indicate that ankaramite was extruded at three different periods at the north-eastern end of the island, either as lava flows or pyroclastic deposits. Cycles of volcanic activity, in which the earlier lavas are ankaramite and t...
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Language: | English |
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Cambridge University Press (CUP)
1955
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Online Access: | http://dx.doi.org/10.1017/s0016756800063421 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800063421 |
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crcambridgeupr:10.1017/s0016756800063421 2024-03-03T08:45:54+00:00 The Geology of North-East Jan Mayen Nicholls, G. D. 1955 http://dx.doi.org/10.1017/s0016756800063421 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800063421 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 92, issue 2, page 127-140 ISSN 0016-7568 1469-5081 Geology journal-article 1955 crcambridgeupr https://doi.org/10.1017/s0016756800063421 2024-02-08T08:41:21Z Abstract Field observations collected on a short expedition to Jan Mayen indicate that ankaramite was extruded at three different periods at the north-eastern end of the island, either as lava flows or pyroclastic deposits. Cycles of volcanic activity, in which the earlier lavas are ankaramite and the later ones trachybasaltic, have been recognized. Article in Journal/Newspaper Jan Mayen Cambridge University Press Jan Mayen Geological Magazine 92 2 127 140 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Nicholls, G. D. The Geology of North-East Jan Mayen |
topic_facet |
Geology |
description |
Abstract Field observations collected on a short expedition to Jan Mayen indicate that ankaramite was extruded at three different periods at the north-eastern end of the island, either as lava flows or pyroclastic deposits. Cycles of volcanic activity, in which the earlier lavas are ankaramite and the later ones trachybasaltic, have been recognized. |
format |
Article in Journal/Newspaper |
author |
Nicholls, G. D. |
author_facet |
Nicholls, G. D. |
author_sort |
Nicholls, G. D. |
title |
The Geology of North-East Jan Mayen |
title_short |
The Geology of North-East Jan Mayen |
title_full |
The Geology of North-East Jan Mayen |
title_fullStr |
The Geology of North-East Jan Mayen |
title_full_unstemmed |
The Geology of North-East Jan Mayen |
title_sort |
geology of north-east jan mayen |
publisher |
Cambridge University Press (CUP) |
publishDate |
1955 |
url |
http://dx.doi.org/10.1017/s0016756800063421 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800063421 |
geographic |
Jan Mayen |
geographic_facet |
Jan Mayen |
genre |
Jan Mayen |
genre_facet |
Jan Mayen |
op_source |
Geological Magazine volume 92, issue 2, page 127-140 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800063421 |
container_title |
Geological Magazine |
container_volume |
92 |
container_issue |
2 |
container_start_page |
127 |
op_container_end_page |
140 |
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1792501580474351616 |