Highly evolved hypabyssal kimberlite sills from Wemindji, Quebec, Canada: insights into the process of flow differentiation in kimberlite magmas

Bibliographic Details
Published in:Contributions to Mineralogy and Petrology
Main Authors: Zurevinski, Shannon E., Mitchell, Roger H.
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2010
Subjects:
Geochemistry and Petrology
Geophysics
Canada
Wemindji
Online Access:http://dx.doi.org/10.1007/s00410-010-0561-8
http://link.springer.com/content/pdf/10.1007/s00410-010-0561-8.pdf
http://link.springer.com/article/10.1007/s00410-010-0561-8/fulltext.html
http://link.springer.com/content/pdf/10.1007/s00410-010-0561-8
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spelling crspringernat:10.1007/s00410-010-0561-8 2023-05-15T18:43:25+02:00 Highly evolved hypabyssal kimberlite sills from Wemindji, Quebec, Canada: insights into the process of flow differentiation in kimberlite magmas Zurevinski, Shannon E. Mitchell, Roger H. 2010 http://dx.doi.org/10.1007/s00410-010-0561-8 http://link.springer.com/content/pdf/10.1007/s00410-010-0561-8.pdf http://link.springer.com/article/10.1007/s00410-010-0561-8/fulltext.html http://link.springer.com/content/pdf/10.1007/s00410-010-0561-8 en eng Springer Science and Business Media LLC http://www.springer.com/tdm Contributions to Mineralogy and Petrology volume 161, issue 5, page 765-776 ISSN 0010-7999 1432-0967 Geochemistry and Petrology Geophysics journal-article 2010 crspringernat https://doi.org/10.1007/s00410-010-0561-8 2022-01-04T07:27:48Z Article in Journal/Newspaper Wemindji Springer Nature (via Crossref) Canada Wemindji ENVELOPE(-78.816,-78.816,53.000,53.000) Contributions to Mineralogy and Petrology 161 5 765 776
institution Open Polar
collection Springer Nature (via Crossref)
op_collection_id crspringernat
language English
topic Geochemistry and Petrology
Geophysics
spellingShingle Geochemistry and Petrology
Geophysics
Zurevinski, Shannon E.
Mitchell, Roger H.
Highly evolved hypabyssal kimberlite sills from Wemindji, Quebec, Canada: insights into the process of flow differentiation in kimberlite magmas
topic_facet Geochemistry and Petrology
Geophysics
format Article in Journal/Newspaper
author Zurevinski, Shannon E.
Mitchell, Roger H.
author_facet Zurevinski, Shannon E.
Mitchell, Roger H.
author_sort Zurevinski, Shannon E.
title Highly evolved hypabyssal kimberlite sills from Wemindji, Quebec, Canada: insights into the process of flow differentiation in kimberlite magmas
title_short Highly evolved hypabyssal kimberlite sills from Wemindji, Quebec, Canada: insights into the process of flow differentiation in kimberlite magmas
title_full Highly evolved hypabyssal kimberlite sills from Wemindji, Quebec, Canada: insights into the process of flow differentiation in kimberlite magmas
title_fullStr Highly evolved hypabyssal kimberlite sills from Wemindji, Quebec, Canada: insights into the process of flow differentiation in kimberlite magmas
title_full_unstemmed Highly evolved hypabyssal kimberlite sills from Wemindji, Quebec, Canada: insights into the process of flow differentiation in kimberlite magmas
title_sort highly evolved hypabyssal kimberlite sills from wemindji, quebec, canada: insights into the process of flow differentiation in kimberlite magmas
publisher Springer Science and Business Media LLC
publishDate 2010
url http://dx.doi.org/10.1007/s00410-010-0561-8
http://link.springer.com/content/pdf/10.1007/s00410-010-0561-8.pdf
http://link.springer.com/article/10.1007/s00410-010-0561-8/fulltext.html
http://link.springer.com/content/pdf/10.1007/s00410-010-0561-8
long_lat ENVELOPE(-78.816,-78.816,53.000,53.000)
geographic Canada
Wemindji
geographic_facet Canada
Wemindji
genre Wemindji
genre_facet Wemindji
op_source Contributions to Mineralogy and Petrology
volume 161, issue 5, page 765-776
ISSN 0010-7999 1432-0967
op_rights http://www.springer.com/tdm
op_doi https://doi.org/10.1007/s00410-010-0561-8
container_title Contributions to Mineralogy and Petrology
container_volume 161
container_issue 5
container_start_page 765
op_container_end_page 776
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