黑龙江金场沟区铜钼矿成矿地质条件分析  

The Analysis About the Geological Conditions of Copper Molybdenum Ore in Jinchanggou,Heilongjiang Province

作　　者：黄广平[1] 杨增武[1] 董传统[1] 

机构地区：[1]黑龙江省有色金属地质勘查702队,黑龙江牡丹江157021

出　　处：《黄金科学技术》2007年第3期24-27,共4页Gold Science and Technology

摘　　要：通过对金场沟铜钼矿床的地质特征分析认为,地层初始矿源层,构造为矿液运移提供了通道和赋矿空间,来自深源和幔源的花岗闪长斑岩的侵入并携带大量矿质,从而形成与花岗闪长斑岩有关的角砾岩型矿床岩浆岩条件分析,We investigated the geologic feature of Jinchanggou copper-milybdenum ore and learned that the primary source bed of stratum and structure supplied channelway and occurrence space for ore fluid travel . The grano（lioriteporphyry intrusion from mantle or anatectic origin carried much mineralized material and the material stored at appropriate mineral-forming condition , consequently breccia deposits formed.

关 键 词：金场沟 铜钼矿 岩浆 地质条件 

分 类 号：P618.41[天文地球—矿床学] P618.65[天文地球—地质学]