摘要
Abstract
The mining area is located in the late Caledonian orogenic system of Qinqi-Kun,and the metallogenic belt belongs to the Pb,Zn and Sn(Cu)metallogenic sub-belt of the Dashian-Shdorong Indochinese epoch,which has good metallogenic conditions.The NW fault in the mine is the main ore-controlling structure and controls the distribution of plagioelongated granite porphyry,which is closely related to the mineralization of copper polymetallic ore bodies,and its primary halo is roughly Cu(Au)-Cu+Mo-Mo+Cu-Mo zoning in the vertical direction.There are roughly Mo-Cu+Mo-Cu-Pb(Pb)+Zn zonings from the center of the porphyry in the lateral direction,and 69 copper and molybdenum deposits are delineated around the primary halo zonings of the porphyry.According to the regional mineral distribution,the metallogenic regularity of Jiadang root shows the trend from high temperature to middle temperature to low temperature,which has huge mineral resource potential.关键词
东昆仑造山带/加当根铜多金属矿/地质特征/找矿前景Key words
East Kunlun orogenic belt/Gadangen copper polymetallic ore/Geological characteristics/Prospecting prospect分类
天文与地球科学
