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The Wolf property - 1998 update: Volcanogenic massive sulphides hosted by...
The Wolf property is situated within the Pelly Mountains, 90 km south of Ross River, Yukon. The Mississippian felsic volcanic and sedimentary rocks which underlie the Wolf...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Tin-bearing skarns of the Thirtymile Range, NTS Sheet 105 C/9: A progress report
This report summarizes the results of geological mapping of the Thirtymile Range, Sheet 105 C/9, and an investigation of tin skarns at the Mindy (MINFILE 105 C 054) and Ork...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Using GIS as a method of identifying controls on the distribution of...
The following paper outlines a method of identifying controls on the distribution of postglacial alpine sediments in the Selwyn Mountains using a Geographic Information System...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Wolf Lake project: Revision mapping of Dorsey Terrane assemblages in the...
The northern half of the Jennings River (104O) and southern half of the Wolf Lake (105B) map areas include polydeformed and metamorphosed rocks of the eastern Big Salmon Complex...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The Skukum Volcanic Complex, 105 D SW: Geology and comparison to the Bennett...
Several centres of continental volcanism are situated in southern Yukon. Two of these, the Skukum Volcanic Complex and the Bennett Lake Cauldron Complex BLCC are closely...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 -
Ancient Pacific Margin - An update on stratigraphic comparison of potential...
Now in its second year, the Ancient Pacific Margin National Mapping (NATMAP) project continues to make progress in elucidating the stratigraphic framework of Yukon-Tanana...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Stratigraphy and alteration of the White Channel gravel at Dago Hill, a...
The high level bench gravels of the Klondike region were first described by R.G. McConnell. He divided the gravels into two formations; the older and stratigraphically lower...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Structural evolution and controls on gold mineralization at Clear Creek, Yukon
Gold mineralization in the Clear Creek area is associated with ca. 92 Ma Tombstone Plutonic Suite intrusions (TPS) emplaced into metasedimentary rocks of the Neoproterozoic to...Date 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 -
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 with...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 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 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 -
The Harlan property: A new sediment-hosted gold discovery in the Selwyn Basin, Yukon
The Harlan property is a significant new sediment-hosted gold prospect within the Selwyn Basin of east-central Yukon Territory. The property has a large, kilometre-scale surface...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The McMillan Deposit - a stratabound lead-zinc-silver deposit in sedimentary...
The McMillan deposit is in the southern portion of the Logan Mountains, 65 km NE of Watson Lake. It is also referred to as the Quartz Lake deposit. Rocks hosting the deposit...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The Scheelite Dome gold project, central Yukon
La Teko Resources Ltd. acquired the Scheelite Dome gold property from Kennecott Canada Exploration Inc. in 1998. Kennecott had explored the central Yukon property since 1994....Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Magma genesis along an arc-transform transition zone
not_specifiedDate updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Soil Geochemistry above Deeply Weathered Porphyry Deposits in Unglaciated...
Much of west-central Yukon escaped glaciation and is underlain by leached and oxidized, deeply weathered bedrock. Background and anomalous metal values in these soils are...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Geology and metamorphic conditions in rocks of the Cassiar Terrane, Glenlyon...
Lower Paleozoic miogeoclinal calcareous rocks of the Cassiar Terrane are intruded by the Early Cretaceous Glenlyon Batholith. Garnet-biotite and garnet-muscovite-biotite-...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML