Post-cumulus disruption of the Lilloise Intrusion, East Greenland
Summary Field, petrographic and chemical evidence from the cumulates of western Lilloise suggest a substantially higher level of exposure in the cumulus pile than is seen on the E side, due to relative subsistence of the western half of the intrusion. It is suggested that the subsistence started whi...
Published in: | Geological Magazine |
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Language: | English |
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Cambridge University Press (CUP)
1976
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Online Access: | http://dx.doi.org/10.1017/s0016756800043272 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800043272 |
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crcambridgeupr:10.1017/s0016756800043272 2024-03-03T08:44:00+00:00 Post-cumulus disruption of the Lilloise Intrusion, East Greenland Matthews, D. W. 1976 http://dx.doi.org/10.1017/s0016756800043272 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800043272 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 113, issue 3, page 287-296 ISSN 0016-7568 1469-5081 Geology journal-article 1976 crcambridgeupr https://doi.org/10.1017/s0016756800043272 2024-02-08T08:32:09Z Summary Field, petrographic and chemical evidence from the cumulates of western Lilloise suggest a substantially higher level of exposure in the cumulus pile than is seen on the E side, due to relative subsistence of the western half of the intrusion. It is suggested that the subsistence started while both cumulus pile and the surrounding basalts were still hot and not fully consolidated. When, later, reactivation occurred, the rocks were in a more cohesive state and ‘syenitic’ magma was available for intrusion as discrete sheets and veins. Article in Journal/Newspaper East Greenland Greenland Cambridge University Press Greenland Geological Magazine 113 3 287 296 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Matthews, D. W. Post-cumulus disruption of the Lilloise Intrusion, East Greenland |
topic_facet |
Geology |
description |
Summary Field, petrographic and chemical evidence from the cumulates of western Lilloise suggest a substantially higher level of exposure in the cumulus pile than is seen on the E side, due to relative subsistence of the western half of the intrusion. It is suggested that the subsistence started while both cumulus pile and the surrounding basalts were still hot and not fully consolidated. When, later, reactivation occurred, the rocks were in a more cohesive state and ‘syenitic’ magma was available for intrusion as discrete sheets and veins. |
format |
Article in Journal/Newspaper |
author |
Matthews, D. W. |
author_facet |
Matthews, D. W. |
author_sort |
Matthews, D. W. |
title |
Post-cumulus disruption of the Lilloise Intrusion, East Greenland |
title_short |
Post-cumulus disruption of the Lilloise Intrusion, East Greenland |
title_full |
Post-cumulus disruption of the Lilloise Intrusion, East Greenland |
title_fullStr |
Post-cumulus disruption of the Lilloise Intrusion, East Greenland |
title_full_unstemmed |
Post-cumulus disruption of the Lilloise Intrusion, East Greenland |
title_sort |
post-cumulus disruption of the lilloise intrusion, east greenland |
publisher |
Cambridge University Press (CUP) |
publishDate |
1976 |
url |
http://dx.doi.org/10.1017/s0016756800043272 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800043272 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
East Greenland Greenland |
genre_facet |
East Greenland Greenland |
op_source |
Geological Magazine volume 113, issue 3, page 287-296 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800043272 |
container_title |
Geological Magazine |
container_volume |
113 |
container_issue |
3 |
container_start_page |
287 |
op_container_end_page |
296 |
_version_ |
1792499469195935744 |