Petrology of the Whitestone Anorthosite

Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/30030

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DC Field	Value	Language
dc.contributor.advisor	McNutt, R. H.	-
dc.contributor.author	Mason, Ian	-
dc.date.accessioned	2024-08-11T00:28:31Z	-
dc.date.available	2024-08-11T00:28:31Z	-
dc.date.issued	1969-08	-
dc.identifier.uri	http://hdl.handle.net/11375/30030	-
dc.description.abstract	The conclusions of this thesis rest on comprehensive geological, chemical and petrographical analyses of both the Whitestone anorthosite and the contiguous rocks. The anorthosite is believed to have been intruded as a magma of anorthositic composition just after the acme of the last regional metamorphism. Various textural and mineralogical features, ostensibly metamorphic, are interpreted as being due to an extravagantly long magmatic end-game.	en_US
dc.language.iso	en	en_US
dc.subject	rock	en_US
dc.subject	geology	en_US
dc.subject	chemical	en_US
dc.subject	magma	en_US
dc.subject	whitestone	en_US
dc.subject	petrology	en_US
dc.subject	anorthosite	en_US
dc.subject	metamorphic	en_US
dc.title	Petrology of the Whitestone Anorthosite	en_US
dc.type	Thesis	en_US
dc.contributor.department	Geology	en_US
dc.description.degreetype	Thesis	en_US
dc.description.degree	Doctor of Philosophy (PhD)	en_US
Appears in Collections:	Digitized Open Access Dissertations and Theses

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