Peel Plateau and the contiguous east flank of the Richardson Mountains, northeastern Yukon, comprise a relatively unexplored but prospective petroleum basin. Within the Devonian succession of this basin, shale rocks of unit `Cf? are little known...
NGR surveys were originally conducted in the Mayo map area in 1987 and 1988. Stream sediment and water samples were collected from a total of 861 sample sites. A total of 861 original samples were selected for reanalysis. Representative 2 gram...
The industrial minerals and minor metals are reviewed alphabetically. Where applicable, information has been included on mineral types, uses, deposit characteristics, mining methods, producers, market specification, prices, Canadian deposits and...
Local-scale surficial geology mapping was completed as part of a community hazards mapping program coordinated by the Northern Climate ExChange (Yukon Research Centre, Yukon College). This program assesses potential landscape hazards under...
A quantitative gamma-ray spectrometric and aeromagnetic helicopter-borne geophysical survey was completed by Fugro Airborne Surveys. The survey was flown from September 10 to October 14, 2008. The nominal traverse and control line spacings were...
Geological map (1:25 000 scale) of Mount Mye (NTS 105 K/6 NE) and Barwell Lake (NTS 105 K/11 SE) central Yukon, including geological cross-sections, mineral occurrences, isotopic age dates, fossil age determinations and geochemical samples.
The Tantalus Formation developed within confined intermontane river valleys during the late stages of collision and amalgamation of Stikinia and associated arc systems with the North American plate in Upper Jurassic and early Lower Cretaceous...
This report is an updated version of an Open File report (Walton, 1996) describin the geology and geochemistry of gemstone deposits and applicable exploration criteria.Teh 1996 report and this update are both aimed at ecploration geologists and...
