新疆和静县仓呼来沟铜矿地质特征及找矿方向

摘要

新疆和静县仓呼来沟铜矿位于巴伦台-星星峡-旱山离散地体西部、那拉提-红柳河缝合带中部。铜矿化主要分布在闪长玢岩节理面、构造破碎带以及硅化蚀变带中，呈脉状分布。以孔雀石化及黄铜矿化的出现作为直接找矿标志。矿床受构造及侵入岩控制，属热液型铜矿。%Canghulaigou copper deposit is located at the west of Baluntai-Xingxingxia-Hanshan discrete terrane, in the middle of Nalati-Hongliuhe suture zone. Copper mineralization is mainly distributed in the diorite porphyrite joints, tectonic fracture zones and silicification zones, showing nervation distribution. The appearances of Malachite mineralization and brass are the direct prospecting marks. The deposit is controlled by faults and intrusions, belonging to the hydrothermal copper deposit.