易门凤山铜矿床断裂构造地球化学特征  

Study on Features of Fracture Tectonogeochemistry of Fengshan Copper Deposit in Yimen

作　　者：马德云[1] 韩润生[1] 刘伟 

机构地区：[1]昆明理工大学国土系开发与城乡建设系

出　　处：《昆明理工大学学报（理工版）》1999年第1期157-161,共5页Journal of Kunming University of Science and Technology(Natural Science Edition)

摘　　要：研究了易门凤山铜矿床深部的断裂构造地球化学特征，圈出了成矿靶区，取得了较好的预测效果。Based on the features of fracture tectonogeochemistry of Fengshan Copper Deposit in Yimen,Yunnan,some metallogic targets have been enclosed,and good results have been achieved in searching for orebodies.It shows that the method of fracture tectonogeochemistry may predict the prognosis of hidden deposit.

关 键 词：断裂构造 地球化学 隐伏矿床预测 铜矿床 

分 类 号：P618.410.2[天文地球—矿床学] P542.3[天文地球—地质学]