摘要
后长川钨矿大地构造位于北祁连加里东褶皱带东带,系属于祁连成矿带。其成矿与地层、构造、岩浆活动具有一定的相关关系。通过研究本区大地构造背景、成矿地质特征等的研究,初步分析了后长川钨矿的矿床地质特征,探讨了矿床成因、控矿因素。
After Changchuan tungsten ore tectonic is located in the North Qilian Caledonian fold belt east belt, belongs to the Qilian metallogenic belt. The mineralization has a certain relationship with strata, structure, magmatic activities. In this paper, by studying the regional tectonic background, and ore-forming geological characteristics, the author analyzed after ChangChuan tungsten ore deposit geological characteristics, ore deposit genesis and ore-controlling factors are discussed as well.
作者
马振甲
贾天瑞
MA Zhen-jia JIA Tian-rui(Gansu Nonferrous Metals Geological Survey Balyin Mineral Exploration Institute, Balyin 730900, Chin)
出处
《甘肃冶金》
2017年第5期69-72,共4页
Gansu Metallurgy
关键词
钨矿
地质特征
矿床成因
控矿因素
后长川
tungsten ore
geologic features
ore genesis
ore-controlling factors
Houchangchuan
