Crescumulate layering in a gabbroic body on Seiland, northern Norway
Summary The cumulates and crescumulates in the Crescumulate Zone of the Rognsund gabbro are described. The olivine and olivine-clinopyroxene crescumulates contain large dendritic crystals of olivine due to rapid upward growth from cumulus nucleii on the temporary floor of the magma chamber. Crescumu...
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Language: | English |
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Cambridge University Press (CUP)
1972
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Online Access: | http://dx.doi.org/10.1017/s0016756800042813 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800042813 |
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crcambridgeupr:10.1017/s0016756800042813 2024-03-03T08:47:23+00:00 Crescumulate layering in a gabbroic body on Seiland, northern Norway Robins, B. 1972 http://dx.doi.org/10.1017/s0016756800042813 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800042813 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 109, issue 6, page 533-542 ISSN 0016-7568 1469-5081 Geology journal-article 1972 crcambridgeupr https://doi.org/10.1017/s0016756800042813 2024-02-08T08:26:16Z Summary The cumulates and crescumulates in the Crescumulate Zone of the Rognsund gabbro are described. The olivine and olivine-clinopyroxene crescumulates contain large dendritic crystals of olivine due to rapid upward growth from cumulus nucleii on the temporary floor of the magma chamber. Crescumulate growth was accompanied by the bottom accumulation of primocrysts, some of which were enlarged by the normal adcumulus process. The crescumulates are thought to have originated when cumulus crystals sank from a labile environment near the roof of the body into a metastable environment on the floor. Article in Journal/Newspaper Northern Norway Cambridge University Press Norway Seiland ENVELOPE(23.275,23.275,70.430,70.430) Rognsund ENVELOPE(23.044,23.044,70.327,70.327) Geological Magazine 109 6 533 542 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Robins, B. Crescumulate layering in a gabbroic body on Seiland, northern Norway |
topic_facet |
Geology |
description |
Summary The cumulates and crescumulates in the Crescumulate Zone of the Rognsund gabbro are described. The olivine and olivine-clinopyroxene crescumulates contain large dendritic crystals of olivine due to rapid upward growth from cumulus nucleii on the temporary floor of the magma chamber. Crescumulate growth was accompanied by the bottom accumulation of primocrysts, some of which were enlarged by the normal adcumulus process. The crescumulates are thought to have originated when cumulus crystals sank from a labile environment near the roof of the body into a metastable environment on the floor. |
format |
Article in Journal/Newspaper |
author |
Robins, B. |
author_facet |
Robins, B. |
author_sort |
Robins, B. |
title |
Crescumulate layering in a gabbroic body on Seiland, northern Norway |
title_short |
Crescumulate layering in a gabbroic body on Seiland, northern Norway |
title_full |
Crescumulate layering in a gabbroic body on Seiland, northern Norway |
title_fullStr |
Crescumulate layering in a gabbroic body on Seiland, northern Norway |
title_full_unstemmed |
Crescumulate layering in a gabbroic body on Seiland, northern Norway |
title_sort |
crescumulate layering in a gabbroic body on seiland, northern norway |
publisher |
Cambridge University Press (CUP) |
publishDate |
1972 |
url |
http://dx.doi.org/10.1017/s0016756800042813 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800042813 |
long_lat |
ENVELOPE(23.275,23.275,70.430,70.430) ENVELOPE(23.044,23.044,70.327,70.327) |
geographic |
Norway Seiland Rognsund |
geographic_facet |
Norway Seiland Rognsund |
genre |
Northern Norway |
genre_facet |
Northern Norway |
op_source |
Geological Magazine volume 109, issue 6, page 533-542 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800042813 |
container_title |
Geological Magazine |
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109 |
container_issue |
6 |
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533 |
op_container_end_page |
542 |
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1792503559755923456 |