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Ultrahigh frequency radio echo sounding of Yukon glaciers
not_specifiedDate updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The setting of the volcanogenic massive sulphide deposits in the Finlayson...
The definition of regionally extensive stratigraphy in deformed and metamorphosed rocks of the Yukon-Tanana Terrane in the Finlayson Lake district allows the recognition of at...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Volcanic-hosted epithermal gold-sulphide mineralization and associated...
The upper Sixtymile River area is located approximately 128 km west of Dawson City, Yukon. Lithology in this area consists of Precambrian to Paleozoic metamorphic rocks,...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Volcanogenic iron and base metal occurrences in Klondike Schist
The term "Klondike Schist" describes metamorphosed igneous and sedimentary rocks first described from the Klondike area and later from south central Yukon. This paper describes...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Trace ammonium in granites of the southern Yukon and its petrogenetic significance
This reconnaissance study compares the ammonium content of some granites from the southern Yukon with granites in other regions. Analyses show a slight variation in ammonium...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Yukon Mining and Exploration Overview 1997
Yukon Exploration and Geology 1997: Mining and Exploration Overview is published as a stand-alone report as well as within the larger publication Yukon Exploration and Geology...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Wolverine Massive Sulfide Project, Yukon
The Wolverine massive sulfide project lies within the Finlayson belt, an elongate composite body bound on the southwest by the Tintina Fault zone and on the northeast by the...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 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 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 Whitehorse (NTS 105D/11), Yukon (1:50 000 scale)
not_specifiedDate updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The Origin and Setting of Anomalous Arc Magmatism in the Wrangell Volcanic...
In the Wrangell Volcanic Belt (WVB) a northwesterly increase in volume of calc-alkaline versus transitional (sodic alkaline/calc-alkaline) magmatism is accompanied by a...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Distal micro-tephra deposits in southeast Alaskan peatlands
Volcanic ash (tephra) provides a valuable tool in palaeoenvironmental research. Traditionally, the main emphasis in tephra studies has been on layers which are visible to the...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
The Vangorda deposit
The Vangorda deposit is a small (7.1 million tonne), SEDEX-type, Pb-Zn-Ag (barite) massive sulphide ore body, in the Anvil District, Yukon, Canada. The deposit is currently...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Tin and tungsten veins and skarns in the McQuesten River area, central Yukon
Tin and tungsten veins and skarns in the McQuesten River area occur in the contact zones of Cretaceous feldpspar-porphyritic biotite granite stocks, plugs, and dykes. Most...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Upper Paleozoic strata with potential for massive sulphide mineralization,...
Northwestern Lansing map area, 120 km east of Mayo, lacks known mineral occurrences yet contains upper Paleozoic stratigraphic units similar to those at volcanic-hosted and...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Stratigraphic framework for syngenetic mineral occurrences, Yukon-Tanana...
Yukon-Tanana Terrane in Grass Lakes map area south of Finlayson Lake consists of highly deformed though regionally mappable metasedimentary and metavolcanic rocks. Four newly...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Stratigraphic succession and U-Pb geochronology from the Teslin suture zone,...
A lithologic succession is recognized in tectonites of the eastern Teslin suture zone in south-central Yukon. Metagraywacke and quartzite, marble, mafic metavolcanics, and...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Stratigraphy and economic potential of Precambrian-Cambrian boundary strata,...
Precambrian-Cambrian boundary strata of the Wernecke Mountains east-central Yukon comprise a succession of alternating carbonate and siliciclastic units. To date only minor...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML