辽宁河坎子钼矿床地质特征及成矿远景预测  

Geological characteristics and mineralization perspective prediction of Hekanzi Mo deposit in Liaoning Province

作　　者：白银增 耿树峰 白云龙 黄志伟 李超 王琦 佟宇 张跃宇 

机构地区：[1]辽宁省有色地质局一0九队,辽宁朝阳122000 [2]吉林大学地球科学院,吉林长春110015

出　　处：《矿产与地质》2017年第5期896-902,共7页Mineral Resources and Geology

基　　金：中央勘查基金项目(2006年);辽宁省本级地质勘查项目(2006年)联合资助成果

摘　　要：辽宁省河坎子钼矿床位于喜峰口—凌源多金属成矿带。从钼矿形成的控矿因素、成矿地质特征、矿床成因入手,分析钼多金属矿区钼矿床形成的主要地质因素、矿床形成的地质作用,预测区内成矿远景,指出河坎子钼矿床为斑岩型矿床,并具大中型矿床成矿远景。Hekanzi Mo deposit is located in Xifengkou-Lingyuan metallogenic belt in Liaoning Province.According to the ore-controlling factors of Mo deposit formation,and geological mineralization characteristics,deposit genesis,the paper has analyzed for the main geological factors and geological function of deposit formation in the Mo polymetallic mining area.It has also predicted for the mineralization perspective in the mining area.It is proposed that HeKanzi Mo deposit is a porphyry type deposit with the mineralization perspective of large-medium-scale deposit.

关 键 词：河坎子钼矿 地质特征 矿床成因 远景预测 辽宁 

分 类 号：P618.65[天文地球—矿床学]