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Geochemistry and PGE mineralization of the Kitto intrusion : a product of Mesoproterozoic plume magmatism through fault bounded archean crust, East Nipigon Embayment, Northern Ontario
(2007)The Kitto intrusion is a Mesoproterozoic 1117.7 ±1.8 Ma peridotitic to gabbroic intrusion, that formed as a result of plume magmatism and was emplaced along Mesoproterozoic and Archean faults in the East Nipigon Embayment ... -
Geology and alteration associated with the Hamlin Lake VMS system, Shebandowan Greenstone belt, Northwestern Ontario, Canada
(2008)The Hamlin Lake area is located approximately 120 km southwest of the City of Thunder Bay, Ontario within the Shebandowan greenstone belt of the Wawa Subprovince, Superior Province. The purpose of this study was to understand ... -
Lithogeochemistry of the sedimentary stratigraphy and metosomatic alteration in the Musselwhite gold deposit, North Caribou Lake belt, Superior province, Canada : implications for deposition and mineralization
(2008)The Musselwhite gold deposit, 100% owned and operated by Goldcorp Inc., has cumulatively produced in excess of 2 million ounces since opening in 1997 and has a projected mine life through 2013. It is situated in the North ... -
Mineralization and tectonic setting of the Norton Lake Region, Uchi subprovince
(2005)The Norton Lake region is located approximately 50 km northeast of Fort Hope within the northernmost unnamed assemblage of the Miminiska-Fort Hope greenstone belt of the Uchi Subprovince, northwestern Ontario. An ... -
Stable isotope (N,O,H) geochemistry, petrology and compositions of biotite of the Musselwhite Mine, Ontario : implications for mineralisation
(2008)Musselwhite mine is located 480 km. north of Thunder Bay, Northwestern Ontario on the southern shores of Opapimiskan Lake in the North Caribou Lake greenstone belt. It is classified as an orogenic gold deposit. -
Whole rock geochemistry, mineral chemistry, petrology and Pt, Pd mineralization of the Seagull Intrusion, Northwestern Ontario
(2005)The Seagull Intrusion emplaced during formation of the 1.1 Ga Mid-continental Rift centred around Lake Superior was studied in several drill core and surface samples and consists of a lower ultramafic section (~650 m) and ...
