摘要
对大溶溪白钨矿床成矿地质特征和富集条件进行了分析 ,并指出成矿作用是在含钨建造钨初始富集的基础上 ,在花岗岩侵入产生的巨大热力驱动下发生的。特定层位和岩体是其成矿的必要条件 ,属似矽卡岩型白钨矿床。矿区与外围以及岩体周边具有发现同类型白钨矿床的前景。
Geological feature and enrichment condition of scheelite deposit at Darongxi were analyzed.Their mineralogenetic function was generated by very largy heat power formed by intrusive granite at base of inital enrichment of scheelite.The body and special stratigraphic horizon were need mineralogentic condition of scheelite deposit.It should belong skarnoid deposit.Same type deposits may be found in mineral district and near the district.
出处
《湖南冶金》
2000年第1期22-26,共5页
Hunan Metallurgy
关键词
地质特征
成矿条件
自钨矿床
Darongxi,scheelite,geological feature,enrichment condition
