THE GASPORT DOLOMITE IN THE VICINITY OF HAMILTON, ONTARIO

Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/31904

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DC Field	Value	Language
dc.contributor.advisor	Armstrong, H. S.	-
dc.contributor.advisor	Best, R. V.	-
dc.contributor.author	Spurgeon, Ernest S.	-
dc.date.accessioned	2025-07-03T22:24:06Z	-
dc.date.available	2025-07-03T22:24:06Z	-
dc.date.issued	1955-05	-
dc.identifier.uri	http://hdl.handle.net/11375/31904	-
dc.description.abstract	The Silurian Gasport dolomite member was studied in the Hamilton area. In spite of the mask ing effect of dolomitization, the stratigraphic re lations and results of petrographic and sedimentalogi- cal examination suggest that the depositional locus was that of a shelf or bank. A thin layer of jarosite was observed; further study may show this layer to have important stratigraphic time value.	en_US
dc.language.iso	en	en_US
dc.subject	Dolomite	en_US
dc.subject	Silurian Period	en_US
dc.subject	Stratigraphy	en_US
dc.subject	Jarosite	en_US
dc.title	THE GASPORT DOLOMITE IN THE VICINITY OF HAMILTON, ONTARIO	en_US
dc.title.alternative	THE GASPORT DOLOMITE	en_US
dc.type	Thesis	en_US
dc.contributor.department	Geology	en_US
dc.description.degreetype	Thesis	en_US
dc.description.degree	Master of Science (MSc)	en_US
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