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Showing 1 to 4 of 4 for “"Glennie domain"”.
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Structural study of the auriferous Santoy shear zone, northeastern Glennie domain, Saskatchewan
… lies within the Pine Lake Greenstone belt of the Glennie domain, 125 km northeast of LaRonge, SK. The Santoy shear zone hosts the Santoy 7, Santoy 8/8 East, and “Santoy Gap” gold deposits. This shear zone was studied using a structural and geochronological (ID-TIMS) approach in order to decipher …
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Structural analysis of the north-central Glennie Domain and controls on gold mineralization in the Santoy Gap Hanging Wall deposit, Seabee area, northern Saskatchewan
The Glennie Domain of northern Saskatchewan, centrally located within the Reindeer zone of the 1.9-1.8 Ga Tans-Hudson orogen, is a poly-deformed terrane with evidence of at least four phases of ductile deformation and resultant complex fold interference patterns. The domain also hosts the only …
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Multi-stage orogenic gold mineralization of the Pine Lake greenstone belt: evidence from the Seabee Gold Operation, Trans-Hudson orogen, northern Saskatchewan
… the Pine Lake greenstone belt, hosted within the Glennie domain of the larger Paleoproterozoic Trans-Hudson orogen. At the Seabee Gold Operation, auriferous quartz veins are hosted within shear zones, such as the Santoy shear system, that are focussed along basalt-intrusion contacts, extending …
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CHARACTERIZING THE AURIFEROUS SYSTEM AT PORKY LAKE WITHIN THE PINE LAKE GREENSTONE BELT, NORTHERN SASKATCHEWAN, WITH A FOCUS ON PETROGRAPHY AND MINERAL CHEMISTRY
Gold mineralization occurs within the Pine Lake greenstone belt in several known and prospective deposits in northern Saskatchewan, Canada. The mineralization systematics at some of these locations within the Seabee Gold Operation, including the Porky Main and Porky West deposits, are poorly …