Geochemistry of a silver-lead-zinc hydrothermal system : ore genesis for the McKay Hill and Horseshoe Hill silver claims in Yukon, Canada

• Main Author: Lara, Hernan Javier
• Other Authors: Nicholson, Kirsten N.
• Language: unknown
• Published: 2017
• Subjects: Silver ores > Yukon > Ogilvie Mountains > Composition; Hydrothermal alteration > Yukon > Ogilvie Mountains; Geochemistry > Yukon > Ogilvie Mountains; Yukon; Canada; Gulch; Selwyn; Ogilvie; Ogilvie Mountains; Wernecke; Dublin Gulch; McQuesten
• Online Access: http://cardinalscholar.bsu.edu/handle/20.500.14291/200712; https://hdl.handle.net/20.500.14291/200712; http://liblink.bsu.edu/uhtbin/catkey/1851712

McKay Hill is located in the Ogilvie Mountains, 50 km north of Keno City, Yukon, Canada. The Wernecke Supergroup was deformed by Late Jurassic and Early Cretaceous arc magmatism and orogeny. Mineral phase identification was performed on 14 ore and 15 gangue samples from McKay Hill and Horseshoe Hill...