The petrology of gabbroic sills in the volcanic series of Roy and McKenzie Townships, Chibougamau Region, Quebec.
Metadiabase sills constitute up to 27 percent of a steeply-dipping assemblage of ancient volcanic rocks in Roy and McKenzie townships, Chibougamau region, northwest Quebec. Three rock types are represented. They are, from lower to upper parts of the sills, metapyroxenite, metadiabase, and diabase-pe...
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McGill University
1957
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ndltd-LACETR-oai-collectionscanada.gc.ca-QMM.1111792014-02-13T03:48:52ZThe petrology of gabbroic sills in the volcanic series of Roy and McKenzie Townships, Chibougamau Region, Quebec.Horscroft, Frank. D.Geological Sciences.Metadiabase sills constitute up to 27 percent of a steeply-dipping assemblage of ancient volcanic rocks in Roy and McKenzie townships, Chibougamau region, northwest Quebec. Three rock types are represented. They are, from lower to upper parts of the sills, metapyroxenite, metadiabase, and diabase-pegmatite. Comparison is made with “metadiorite” and “metagabbro” sills in an adjoining area. Chemical and planimetric analyses show that layering of the sills is the result of magmatic differentiation which is characterized by iron-enrichment. The metadiabase sills are similar to the intrusive phase of plateau-type basaltic magma in chemical composition and in trend of differentiation.McGill UniversityKranck, E. (Supervisor)1957Electronic Thesis or Dissertationapplication/pdfenalephsysno: NNNNNNNNNTheses scanned by McGill Library.All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.Doctor of Philosophy. (Department of Earth Sciences.) http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=111179 |
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en |
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Geological Sciences. |
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Geological Sciences. Horscroft, Frank. D. The petrology of gabbroic sills in the volcanic series of Roy and McKenzie Townships, Chibougamau Region, Quebec. |
description |
Metadiabase sills constitute up to 27 percent of a steeply-dipping assemblage of ancient volcanic rocks in Roy and McKenzie townships, Chibougamau region, northwest Quebec. Three rock types are represented. They are, from lower to upper parts of the sills, metapyroxenite, metadiabase, and diabase-pegmatite. Comparison is made with “metadiorite” and “metagabbro” sills in an adjoining area. Chemical and planimetric analyses show that layering of the sills is the result of magmatic differentiation which is characterized by iron-enrichment. The metadiabase sills are similar to the intrusive phase of plateau-type basaltic magma in chemical composition and in trend of differentiation. |
author2 |
Kranck, E. (Supervisor) |
author_facet |
Kranck, E. (Supervisor) Horscroft, Frank. D. |
author |
Horscroft, Frank. D. |
author_sort |
Horscroft, Frank. D. |
title |
The petrology of gabbroic sills in the volcanic series of Roy and McKenzie Townships, Chibougamau Region, Quebec. |
title_short |
The petrology of gabbroic sills in the volcanic series of Roy and McKenzie Townships, Chibougamau Region, Quebec. |
title_full |
The petrology of gabbroic sills in the volcanic series of Roy and McKenzie Townships, Chibougamau Region, Quebec. |
title_fullStr |
The petrology of gabbroic sills in the volcanic series of Roy and McKenzie Townships, Chibougamau Region, Quebec. |
title_full_unstemmed |
The petrology of gabbroic sills in the volcanic series of Roy and McKenzie Townships, Chibougamau Region, Quebec. |
title_sort |
petrology of gabbroic sills in the volcanic series of roy and mckenzie townships, chibougamau region, quebec. |
publisher |
McGill University |
publishDate |
1957 |
url |
http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=111179 |
work_keys_str_mv |
AT horscroftfrankd thepetrologyofgabbroicsillsinthevolcanicseriesofroyandmckenzietownshipschibougamauregionquebec AT horscroftfrankd petrologyofgabbroicsillsinthevolcanicseriesofroyandmckenzietownshipschibougamauregionquebec |
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1716639567202746368 |