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...

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Bibliographic Details
Published in:Geological Magazine
Main Author: Matthews, D. W.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1976
Subjects:
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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spelling 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
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