Hollow apatites in a layered basic intrusion, Norway

Summary Cumulate apatite crystals with infilled tube-like cavities parallel to the c -axis are described from a layered gabbro intrusion in Northern Norway. These are considered to be skeletal crystals produced by rapid growth in the supercooled roof zone of the magma chamber. At least two stages of...

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Bibliographic Details
Published in:Geological Magazine
Main Author: Gardner, P. M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1972
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800039765
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800039765
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spelling crcambridgeupr:10.1017/s0016756800039765 2024-03-03T08:47:23+00:00 Hollow apatites in a layered basic intrusion, Norway Gardner, P. M. 1972 http://dx.doi.org/10.1017/s0016756800039765 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800039765 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 109, issue 5, page 385-392 ISSN 0016-7568 1469-5081 Geology journal-article 1972 crcambridgeupr https://doi.org/10.1017/s0016756800039765 2024-02-08T08:26:21Z Summary Cumulate apatite crystals with infilled tube-like cavities parallel to the c -axis are described from a layered gabbro intrusion in Northern Norway. These are considered to be skeletal crystals produced by rapid growth in the supercooled roof zone of the magma chamber. At least two stages of growth are suggested on the basis of the morphology of the apatites. The interiors of the crystals contain phases representing the trapped magma or the cumulus mineral phase within which they are enclosed. Recirculation of the apatite primocrysts by convection currents is indicated by the interrupted form of some of the tubes. Article in Journal/Newspaper Northern Norway Cambridge University Press Norway Geological Magazine 109 5 385 392
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
spellingShingle Geology
Gardner, P. M.
Hollow apatites in a layered basic intrusion, Norway
topic_facet Geology
description Summary Cumulate apatite crystals with infilled tube-like cavities parallel to the c -axis are described from a layered gabbro intrusion in Northern Norway. These are considered to be skeletal crystals produced by rapid growth in the supercooled roof zone of the magma chamber. At least two stages of growth are suggested on the basis of the morphology of the apatites. The interiors of the crystals contain phases representing the trapped magma or the cumulus mineral phase within which they are enclosed. Recirculation of the apatite primocrysts by convection currents is indicated by the interrupted form of some of the tubes.
format Article in Journal/Newspaper
author Gardner, P. M.
author_facet Gardner, P. M.
author_sort Gardner, P. M.
title Hollow apatites in a layered basic intrusion, Norway
title_short Hollow apatites in a layered basic intrusion, Norway
title_full Hollow apatites in a layered basic intrusion, Norway
title_fullStr Hollow apatites in a layered basic intrusion, Norway
title_full_unstemmed Hollow apatites in a layered basic intrusion, Norway
title_sort hollow apatites in a layered basic intrusion, norway
publisher Cambridge University Press (CUP)
publishDate 1972
url http://dx.doi.org/10.1017/s0016756800039765
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800039765
geographic Norway
geographic_facet Norway
genre Northern Norway
genre_facet Northern Norway
op_source Geological Magazine
volume 109, issue 5, page 385-392
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800039765
container_title Geological Magazine
container_volume 109
container_issue 5
container_start_page 385
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