摘要
哈西金矿位于哈图金矿西邻,地处安齐断裂上盘并受其控制,主要呈NEE向展布,安齐断裂为矿区的主要构造,主要赋矿地层为石炭系,区内出露大面积酸性岩体.矿脉类型以蚀变岩+石英脉为主,成矿时间为华力西中期,与该区酸性岩体侵入同期,但严格受构造控制.笔者认为本区找矿方向以主构造上盘复合构造部位为重点.
The Ha-Xi Gold Deposit is located on the west of the Ha-Tu Gold Deposit, and occurs in the upper part of and is controlled by the NNE An-Qi Fracture Zone,. The An-Qi Fracture Zone is the main structure in the mining area while the geology is dominated by Carboniferous startigraphy and large areas of acidic rock. Mineralization occurs in altered rock and in quartz veins. The time of mineralization is the Hua Lixi middle period. The author believes that a recombined structure is the most important part for finding ore direction.
出处
《新疆地质》
CAS
CSCD
2005年第1期31-35,共5页
Xinjiang Geology
