摘要
内蒙古林西大井铜锡多金属矿区的矿床类型很特殊 ,其特点是脉薄而密集 ,且多金属复杂共生 ,具有较高的研究价值。通过对矿区的构造特征和矿床特征的分析 ,论述了构造的形成机制 ,进而探讨构造与成矿的关系 ,认为构造在成矿过程中起着重要的作用。
Dajing copper-tin-polymetallic deposit in Inner Mongolia is a special deposit type, and considerable for study. It is characterized by the thinness and compactness of ore-vines, complex paragenetic association of polymetal and their comprehensive exploitation. Through analyzing the characteristics and relationship between structures and mineralization, this paper discusses the formation of structures and reveals that structures play an important role in the processes of mineralization.
出处
《地质与勘探》
CAS
CSCD
北大核心
2001年第5期19-23,共5页
Geology and Exploration
基金
中国科学院"九五"重大项目资助 (课题号KZ95 1-B1- 40 4)
