Rubidium-Strontium Mineral and Rock Ages at Sudbury, Ontario

Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/5667

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DC Field	Value	Language
dc.contributor.advisor	McNutt, R. H.	en_US
dc.contributor.author	Gibbins, Arnold Walter	en_US
dc.date.accessioned	2014-06-18T16:32:34Z	-
dc.date.available	2014-06-18T16:32:34Z	-
dc.date.created	2009-08-06	en_US
dc.date.issued	1973-09	en_US
dc.identifier.other	opendissertations/1014	en_US
dc.identifier.other	1584	en_US
dc.identifier.other	927612	en_US
dc.identifier.uri	http://hdl.handle.net/11375/5667	-
dc.description.abstract	<p>Chemical and isotopic results have been used to calculate Rb⁸⁷/Sr⁸⁶ and Sr⁸⁷/Sr⁸⁶ ratios of both whole rock and mineral samples from the Sudbury Area of Northern Ontario. Using these ratios and the principles of radio-active dating, age of various geologic events have been calculated.</p> <p>These ages, along with results of other age dating and geologic studies in the area, are used to examine the origin and history of both the Nickel Irruptive and the Murray Granite. Finally, significant Rb-Sr mineral and whole rock ages from Sudbury and the geologic events they reflect are reviewed in chronological order and correlated with ages and events in adjacent areas.</p>	en_US
dc.subject	Geology	en_US
dc.subject	Geology	en_US
dc.title	Rubidium-Strontium Mineral and Rock Ages at Sudbury, Ontario	en_US
dc.type	thesis	en_US
dc.contributor.department	Geology	en_US
dc.description.degree	Doctor of Philosophy (PhD)	en_US
Appears in Collections:	Open Access Dissertations and Theses

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