摘要
小柳沟铜钨矿矿床成因类型属层控改造型 ,在其形成过程中 ,各种地质因素相互配合 ,相互作用 ,共同制约着矿体的分布特征、形态产状、规模、品位及其矿物组合。在诸多的控矿地质因素中 ,有利的地层单元是成矿的前提基础 ,适宜的岩石构造环境是成矿的必要场所 ,充分的岩浆岩条件是成矿的动力源泉。
The Xiaoliugou Cu-W deposit is controlled by strata and has been rebuilt in late time. During forming stage, various geological factors controlled ore distribution, forming-scale, grade and mineral assemblages. In the all geological factors, the stratum cell was precondition of mineralization. Suitable petrology-structure environments were essential condition. Magmatic activities were dynamic sources for mineralization.
出处
《地质与勘探》
CAS
CSCD
北大核心
2002年第4期33-35,40,共4页
Geology and Exploration
