Felsic magmatic phases and the role of late-stage aplitic dykes in the formation of the world-class Cantung Tungsten skarn deposit, Northwest Territories, Canada-Reference-Cited by-同舟云学术

Felsic magmatic phases and the role of late-stage aplitic dykes in the formation of the world-class Cantung Tungsten skarn deposit, Northwest Territories, Canada

Published:2011-10 Issue:1 Volume:41 Page:75-111
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Rasmussen Kirsten L.,Lentz David R.,Falck Hendrik,Pattison David. R.M.

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference138 articles.

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2. Carcajou Canyon map-area, District of Mackenzie, Northwest Territories;Aitken;Geological Survey of Canada Paper,1974

3. Aitken, J.D., Cook, D.G., Yorath, C.J., 1982. Upper Ramparts River (106G) and Sans Sault Rapids (106H) map areas, District of Mackenzie. Geological Survey of Canada Memoir 388.

4. Technological Assessment Report of Canada Tungsten Mining Corporation Limited, Tungsten;Report,1983

5. Selwyn plutonic suite and its relationship to tungsten skarn mineralization, southeastern Yukon and District of Mackenzie;Anderson,1983

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