Geology, mineral equilibria, sulfur, rubidium-strontium and lead isotopes and intrusion chemistry of the McDame tungsten skarn prospect, north central British Columbia
The McDame tungsten skarn prospect occurs in Hadrynian to Ordovician clastic and carbonate metasediments near Cretaceous felsic stocks. Three prograde skarn and ore facies and one retrograde facies are 1ithologically and structurally controlled. Prograde massive calcsilicate W-MO-Fe facies, characte...
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| Language: | English |
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University of British Columbia
2010
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| Online Access: | http://hdl.handle.net/2429/24563 |