新疆沙尔布拉克金矿床成因矿物学成矿模式  

GENETIC MINERALOGY AND METALLOGENTC MODEL OF SHAERBULAKE GOLD DEPOSIT IN XINJIANG

作　　者：方耀奎[1] 

机构地区：[1]成都理工学院应用化学系

出　　处：《地球科学（中国地质大学学报）》1996年第3期320-326,共7页Earth Science-Journal of China University of Geosciences

基　　金：新疆地矿局科研项目

摘　　要：通过沙尔布拉克金矿床标型矿物组合中黄铁矿、毒砂及石英的化学成分、矿物包裹体及同位素等标型特征及时空演化的研究。The study on typomorphic peculiarities such as chemical composition, fluid inclusions, stable isotope and time space evolution of pytite, quartz and arsenopyrite from Shaerbulake gold deposit in Xinjiang suggests that the mineralization mechanism of the deposit is percolating of thermal mine in the rocks. Thus, a genetic model is presented.

关 键 词：金矿床 成因 矿物学 成矿模式 

分 类 号：P618.510.1[天文地球—矿床学]