Abstract

The Tianger gold deposit occurs in the E-W trending Tianger shear zone in the west Tianshan Mountains, Xinjiang Province. The ore — body is mainly composed of mylonitized granite, and mylonitized sulfide-quartz veins. Highly strained zones within the shear zone are the main pathways through which gold was remobilized. The gold — pyrrhotite — pyrite — quartz vein stage is the most important gold-forming period. The REE contents in mylonitized granites are much higher than those of quartz veins. The gold-bearing rocks are clearly LREE-enriched and Eu-depleted. Au, Ag and As were deposited simultaneously during ore formation.

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