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THE GASPORT DOLOMITE IN THE VICINITY OF HAMILTON, ONTARIO

dc.contributor.advisorArmstrong, H. S.
dc.contributor.advisorBest, R. V.
dc.contributor.authorSpurgeon, Ernest S.
dc.contributor.departmentGeologyen_US
dc.date.accessioned2025-07-03T22:24:06Z
dc.date.available2025-07-03T22:24:06Z
dc.date.issued1955-05
dc.description.abstractThe 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.description.degreeMaster of Science (MSc)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/31904
dc.language.isoenen_US
dc.subjectDolomiteen_US
dc.subjectSilurian Perioden_US
dc.subjectStratigraphyen_US
dc.subjectJarositeen_US
dc.titleTHE GASPORT DOLOMITE IN THE VICINITY OF HAMILTON, ONTARIOen_US
dc.title.alternativeTHE GASPORT DOLOMITEen_US
dc.typeThesisen_US

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