吉林省岩浆铜镍硫化物矿床地质特征及成矿模式  

Geological Characteristics and Mlnerogenetic Pattern of Magmatic Cu-Ni Sulphide Depsits in Jilin

作　　者：陈子诚 

机构地区：[1]中国有色金属工业总公司吉林地质勘查局

出　　处：《地质与勘探》1991年第10期1-10,共10页Geology and Exploration

摘　　要：吉林省是我国岩浆铜镍硫化物矿床的矿化集中区之一.本文总结了该省基性、超基性岩体及铜镍矿床赋存的大地构造环境,阐明了深断裂对岩体和矿床的控制作用,岩体及矿床地质特征,以及矿床成因、成矿作用和成矿模式.Jilin is one of the provinces crowded with magmatic Cu Ni sulphide deposits (mineralizations) in cur country. This paper sums up the tectcnic setting for the cccurrence of basic-ultrabasic rocks and Cu Ni deposits, and expcunds the author's views on following questions, including: the control of deep fracturcs on mincral deposits, geological characteristics, genesis, metallogcncsis and minerogenctic pattern.

关 键 词：铜 镍 硫化物 矿床 地质 成矿 

分 类 号：P618.410.5[天文地球—矿床学]