摘要
本文简述了沙柳河南区有色金属矿床的基本特征。通过对成矿热液及成矿物质的来源与性质的研究,认为该矿床的成因类型为火山沉积—接触交代改造叠加型,进而探讨了该矿床的成矿模式。
Based on a brief introduction of the fundamental characteristics of the Southern Shali-uhe nonferrous metal deposit, through studing the sources and properties of metallogenic hy-drothermal solution and metallogenic materials,the author holds that this deposit should be clas-sified genetically as a volcano-sedimental deposit reformed and superimposed by contact metaso-matism,and,furthermore,gives a discussion on metallogenic model of this deposit.
关键词
青海沙柳河
有色金属矿床
成矿物质来源
成矿模式
Shaliuhe
Qinghai
Nonferrous metal deposit
Source of metallogenic materials
Metallogenic model
