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Summary of the Kudz Ze Kayah Project, Volcanic Hosted Massive Sulphide...
The ABM polymetallic Volcanic Hosted Massive deposit underlies claims within the Kudz Ze Kayah project area. The deposit is a volcanic hosted massive sulphide body within a...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Surficial geology and sedimentology of Garner Creek, Ogilvie and Matson...
The central Yukon Territory has a number of favourable placer deposit settings due to its unique history of multiple glaciations, active stream sedimentation in association...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Surficial geology and till geochemistry of Weasel Lake map area (105G/13),...
Weasel Lake map area (105G/13) is located at the northwestern end of the Finlayson Lake belt (displaced Yukon-Tanana Terrane) and extends northward into ancient North American...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Reconnaissance geology of northern Toobally Lake (95D/8), southeast Yukon
The Toobally fault is a north-trending structure occurring along the west shore of northern Toobally Lake (95D/8) that juxtaposes Neoproterozoic-Cambrian sedimentary and...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Report of 1982 field work on Early Tertiary clastics, west-central Yukon
Eight lithofacies types have been identified. These include: 1) Gms - massive, matrix support conglomerate; 2) Gm - massive or crudely bedded, clast supported conglomerate; 3)...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Surficial Geology of Alligator Lake (NTS 105D/6), Yukon (1:50 000 scale)
not_specifiedDate updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Surficial Geology of Fenwick Creek (NTS 105D/3), Yukon (1:50 000 scale)
not_specifiedDate updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Surficial Geology of MacRae (NTS 105D/10), Yukon (1:50 000 scale)
not_specifiedDate updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Surficial Geology of Robinson (NTS 105D/7), Yukon (1:50 000 scale)
not_specifiedDate updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Surficial Geology of Whitehorse (NTS 105D/11), Yukon (1:50 000 scale)
not_specifiedDate updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Syn-mineralization faults and their re-activation, Finlayson Lake massive...
Although deformed and metamorphosed, the strata hosting volcanogenic massive sulphide deposits in the Finlayson Lake district retain characteristics that suggest the influence...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Taiga property: A stratiform Ni-Zn-PGE target in north-central Yukon
The Taiga property consists of 1043 claims located 95 km northeast of Dawson and 6 km east of the Dempster Highway. Ordovician to Silurian Road River Group dolomite and black...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Tectonic significance of plutonism in the Thirtymile Range, southern Yukon
Two distinct but undeformed suites of granitic plutons intrude deformed siliciclastic rocks in western Dorsey Terrane. A calc-alkaline hornblende-bearing gabbro to granodiorite...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Textural characteristics of the Venus vein and implications for ore shoot...
Underground observations indicate Venus formed from hydrothermal solutions by both open space filling and replacement processes. Quartz deposition was ubiquitous throughout the...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The Carmacks Hydrothermal Event: An Alteration Study in the Southern Dawson...
Gold-rich polymetallic vein deposits, and gold-copper porphyry deposits, occur along a northwesterly trend across the southern Dawson Range. Vein mineralization is hosted by...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The exotic nature of the Last Peak eclogite in the Teslin zone,...
The history of an eclogite sample and a mica schist sample from the western Teslin zone are discussed in view of garnet zoning profiles. The preliminary metamorphic results...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The Fer property: A plutonic-related gold property in southeastern Yukon
The Fer gold property lies only 5 kilometres southwest of the Nahanni Range Road (Highway 10) in southeastern Yukon. It is underlain by a broadly folded sequence of coarse...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The Fyre Lake Deposit: A New Copper-Cobalt-Gold VMS Discovery
The Fyre Lake volcanogenic massive sulphide (VMS) copper-cobalt-gold property is situated 160 kilometres northwest of Watson Lake in the Finlayson Lake area of the Yukon-Tanana...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The Fyre Lake project 1997: Geology and mineralization of the Kona massive...
Columbia Gold Mines Fyre Lake project is located immediately to the east of Fire Lake, approximately 160 km north of Watson Lake in the Yukon Territory. The 1997 program,...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The geology of placer gold deposits in the Indian River area, west-central Yukon
Placer gold deposits in the Indian River area, west-central Yukon, are grouped into five classes based on thickness, grain size, composition, age, process, landform and...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML