金川Ⅰ矿区6#富铜盲矿体成因探讨  

A STUDY ON THE GENESIS OF BLIND OREBODY RICH IN 6# CU OF OREFIELD Ⅰ, JINCHUAN

作　　者：孟蓉[1] 田毓龙[1] 

机构地区：[1]昆明理工大学,云南昆明650093

出　　处：《云南地质》2006年第3期374-380,共7页Yunnan Geology

摘　　要：金川硫化铜镍矿床Ⅰ矿区6#富铜矿属于岩浆深熔-晚期贯入矿体,于正常的超基性岩型富矿体之后,富含贵金属元素和铜镍的富矿岩浆沿北东东向张性断裂上侵形成,呈透镜状产出。The metallogenesis of orebody rich in Cu of Jinchuan sulfide Cu-Ni deposit belongs to the type of magmatic anatexis-late injection. It is formed after the rich orebody of normal ultrabasic rock type. And the magma rich in precious metal elements and Cu-Ni intrudes upwards along the NEE tensile fault, which is in lenticulated occurrence.

关 键 词：盲矿体 铜镍硫化物矿床 成因 金川 甘肃 

分 类 号：P618.104[天文地球—矿床学]