吉林杨金沟白钨矿床控矿因素及远景预测  

Scheelite deposit ore-controlling factors and prediction in Yangjingou of Jilin Province

作　　者：艾德新 李峰[1] 刘玉平[1] 

机构地区：[1]吉林省有色金属地质勘查局六○三队,珲春133300

出　　处：《长春工程学院学报（自然科学版）》2008年第4期55-58,共4页Journal of Changchun Institute of Technology：Natural Sciences Edition

摘　　要：在对矿区地质背景、矿床地质特征简要阐述的基础上,重点对矿床控矿因素进行了分析,探讨了矿区下古生界五道沟群、华力西晚期至燕山期侵入岩以及主要断裂构造与成矿作用关系,预测了区域内钨矿找矿远景。The paper discussed ore - controlling factors according to the description of geological characteristics. The exploring prediction is put forward through expounding the relation between fracture structure of Wudaogou group of lower palaeozoic Erathem and late Vail-scian stage and mineralization.

关 键 词：白钨矿床 地质特征 控矿因素 远景预测 杨金沟 

分 类 号：P612[天文地球—矿床学]