摘要
沙泉子铜矿是东天山雅满苏-沙泉子铜铁多金属成矿带发现一重要铜矿床。东天山雅满苏晚古生代岛弧带是该矿的大地构造位置所在,区内具有非常突出的断裂构造特征主要为康孤儿以及沙泉子断裂等。区内岩浆活动强烈,断裂构造发育。沙泉子铜矿主要赋存于石炭纪雅满苏岛弧带、下石炭统雅满苏组一套细碧角斑岩建造中。文中笔者主要对该矿地质特征及矿床成因进行分析和探讨,旨在为该区找矿提供指导。
The shaquan Zi copper deposit is an important copper deposit found in the copper iron polymetallic metallogenic belt of the East Tianshan jaan Siu Sha Quan. The late Paleozoic island arc belt in the eastern Tianshan Mountains is the tectonic location of the mine. The area is characterized by prominent fault structures, mainly known as the orphan of the Kang and the Sha Quan Zi fault. The magmatic activity in the area is strong and the fracture structure is developed. The Sha Quan Zi copper deposit is mainly located in the formation of a set of fine blue porphyry in the Carboniferous Jan-Suan island arc belt and the lower Carboniferous Jan-Siu-Su formation. In this paper, the author mainly analyzes and discusses the geological characteristics of the ore and the genesis of the deposit, so as to provide guidance for the prospecting in this area.
作者
周晓飞
ZHOU Xiao-fei1,2(1.The Xinjiang Uygur Autonomous Region Bureau of Geology and mineral resources in Akesu area Turpanxiuke town Turpanxiuke village team,Akesu 843000,China;2.Ninth geological team of the Xinjiang Uygur Autonomous Region geological and mineral exploration and Development Bureau,Urumchi 830000,Chin)
出处
《世界有色金属》
2018年第2期171-172,共2页
World Nonferrous Metals
关键词
沙泉子铜矿
地质特征
矿床成因
Sha Quan Zi copper deposit
geological characteristics
genesis of the deposit
作者简介
周晓飞,男,生于1966年,汉族,陕西丹凤人,本科,高级工程师,研究方向：地质矿产.
