摘要
阿克海哈勒位于西伯利亚板块南阿尔泰晚古生代弧后盆地中段,阿尔泰地槽褶皱系之喀拉额尔齐斯复式背斜的西北端构造尖灭部位。属于阿尔泰南缘Cu-Pb-Zn-Fe-Au-RM-白云母-宝石成矿带北部麦兹-冲乎尔Fe-CuPb-RM-宝石成矿带。成矿地质条件优越。通过1:1万土壤测量研究区共圈出11个综合异常区,经过地表探槽工程验证发现金矿体1条,金矿化体4条,铜、铅、锌矿化体各1条。通过对阿克海哈勒研究区成矿地质条件、地球化学及地球物理条件的综合分析,认为阿克海哈勒通过进一步勘查工作有望找到火山热液型金、铜多金属矿的找矿潜力。
Akhai Hal is located in the middle part of the late Paleozoic back arc basin in the southern Altai plate of the Siberia plate, and the northwest end of the karajar complex anticline in the Altai geosyncline fold system. It belongs to the Metz Chong Er Fe-Cu-Pb-RM-gemstone metallogenic belt in the northern Cu-Pb-Zn-Fe-Au-RM-Muscovite gem metallogenic belt, southern Altai. The metallogenic geological conditions are superior. 11 comprehensive anomaly areas were circled through the 1：1 10000 soil survey research area, and 1 gold ore bodies were found through the surface exploration project, 4 gold orebodies were found, and 1 copper, lead and zinc mineralization bodies were found. Through the comprehensive analysis of the metallogenic geological conditions, geochemistry and geophysical conditions of the akhai Hal research area, it is believed that through further exploration, akhai Halle is expected to find the prospecting potential of the volcanic hydrothermal type gold and copper polymetallic ore.
作者
应元庆
YING Yuan-qing(Xinjiang geology and mineral exploration and Development Bureau Fourth Geological Brigade, Aletai 836500,Chin)
出处
《世界有色金属》
2018年第6期97-98,共2页
World Nonferrous Metals
基金
2016年度中央返还两权价款资金矿产
能源调查评价委托项目(编号A16-2-LQ03)的成果
关键词
地球化学异常
找矿前景
阿克海哈勒
geochemical anomalies
prospecting potential
akhhai Halle
作者简介
应元庆,男,生于1982年,地质矿产工程师,研究方向：地质勘查.
