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Geology, Mount Nansen - Nisling River area, Yukon.

Author: Canadian Electronic Library (Firm)
Publisher: Ottawa : Natural Resources Canada, 2016.
Series: Canadian geoscience map., DesLibris., Documents collection.
Edition/Format:   eBook : Document : National government publication : English
Summary:
The Mount Nansen-Nisling River area is underlain dominantly by Paleozoic rocks of Yukon Tanana terrane, and Triassic to Paleogene successor rocks. Rocks to the east are dominated by the Mississippian Simpson Range suite that is intruded by the voluminous Early Jurassic Long Lakes suite. The western geology is dominated by metasedimentary rocks of the Snowcap assemblage and Stevenson Ridge schist, and lesser  Read more...
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Genre/Form: Electronic books
Material Type: Document, Government publication, National government publication, Internet resource
Document Type: Internet Resource, Computer File
All Authors / Contributors: Canadian Electronic Library (Firm)
ISBN: 9780660055305 0660055309
OCLC Number: 1001209554
Notes: Issued as part of the desLibris documents collection.
Description: 1 online resource ([12] pages).
Details: Mode of access: World Wide Web.
Series Title: Canadian geoscience map., DesLibris., Documents collection.
More information:

Abstract:

The Mount Nansen-Nisling River area is underlain dominantly by Paleozoic rocks of Yukon Tanana terrane, and Triassic to Paleogene successor rocks. Rocks to the east are dominated by the Mississippian Simpson Range suite that is intruded by the voluminous Early Jurassic Long Lakes suite. The western geology is dominated by metasedimentary rocks of the Snowcap assemblage and Stevenson Ridge schist, and lesser Finlayson assemblage metavolcanic and metasedimetary rocks. Permian Sulphur Creek suite forms sparse intrusions of K-feldsparaugen granite. The northern geology is dominated by the mid-Cretaceous Whitehorse plutonic suite and Mount Nansen Group volcanic rocks, that locally host Cu-Au porphyry and Au mineralization. Late Cretaceous Casino suite hypabyssal rocks are present sparsely across much of the area with and have known porphyry and epithermal mineral potential (e.g. Klaza). Paleogene volcanic and hypabys.

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Primary Entity

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