The geological characteristics and metallogenic regularity of red copper gold deposit in Xinjiang and quiet County
WANG Zong-bin;WU Chun-wei;YANG Xiao-fei;FAN Zi-chun;XIE Ri-shi;Xinjiang geological and mineral exploration and Development Bureau Third Geological Brigade;
The red-embankment copper-gold deposit is located in the early Paleozoic continental margin of the Boluookunu, and the tectonic activity in the area is strong, and the development of the intrusive rocks, especially in the late Nalixi, is very favorable. The metallogenic geological conditions are favorable,(D_3a), as a set of gray-gray black thick layer of massive limestone, marble limestone amphibolite quartzite schist, sandstone, siltstone, etc., ore body and more Veined, lenticular form output, smaller scale. The alteration of the surrounding rock is mainly silicification, green petrochemical, chloritization, garnet petrochemical, and a small amount of pyrite mineralization. The deposit belongs to hydrothermal metasomatic deposit.
【CateGory Index】： P618.51