RELATIONSHIP BETWEEN GOLD MINERALIZATION AND STRIKE-SLIP FAULTING IN WULONGGOU MINING DISTRICT, EASTERN KUNLUN MOUNTAINS

摘要

The Wulonggou gold mining district is located in the middle section of the northern zone of the Eastern Kunlun Mountains. The master strata emerged in the northern zone are a set of Precambrian Volcano-sedimentary deep metamorphic petrographic series. The magmatic activities are intense and Frequent in this zone, particularly the intermediate - acid intrusions. The two large boundary fault belts (the North fault belt and the central fault belt) of the northern zone are sinistral strike-slip faulting, which Cause the northern zone to develop the intracontinental dextral shearing movement, and form the NW-trending structural style.