摘要
和静县新C-2007-389号航磁异常区铁铜多金属矿位于阿吾拉勒晚古生代裂谷,属阿吾拉勒铁多金属矿成矿带,区内断裂构造活动强烈,火山岩发育,尤其是以下石炭统大哈拉军山组为主,成矿地质条件十分有利,赋矿岩层主要为下石炭统大哈拉军山组的火山岩,发育孔雀石化、黄铁矿化等。
The iron-copper polymetallic deposit in the new C-2007-389 aeromagnetic anomaly zone is located in the Late Paleozoic rift of the Awu Lalal, which belongs to the Awu Lalite polymetallic mineralization belt. The tectonic activity in the area is strong, Development, especially the following Carboniferous large Hala Junshan group-based, metallogenic geological conditions are very favorable, Fu ore formation mainly for the lower Carboniferous large Hala Jianshan group volcanic rocks, the development of malachite petrochemical, pyrite and so on.
出处
《世界有色金属》
2017年第11期82-83,共2页
World Nonferrous Metals
关键词
航磁异常区铁铜多金属矿
地质特征
找矿标志
aeromagnetic anomalous iron - copper polymetallic ore
geological features
prospecting signs
