The source of hydrothermal fluids for the Sarekoubu gold deposit in the southern Altai, Xinjiang, China: Evidence from fluid inclusions and geochemistry

Volume: 32, Issue: 2, Pages: 247 - 258
Published: Mar 31, 2008
Abstract
null null The Sarekoubu gold deposit, located at the southern margin of the Altai Mountains, Xinjiang, occurs in metamorphic acid volcanic and volcaniclastic rocks of Devonian Kangbutiebao Formation. Echelon-like ore-bearing veins occur as dextrorotation, intersect ore-controlling faults at small angles. Ore-bearing minerals in the vein systems are mainly native gold, electrum, pyrite, pyrrhotite, chalcopyrite, sphalerite, galena, and native...
Paper Details
Title
The source of hydrothermal fluids for the Sarekoubu gold deposit in the southern Altai, Xinjiang, China: Evidence from fluid inclusions and geochemistry
Published Date
Mar 31, 2008
Volume
32
Issue
2
Pages
247 - 258
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