西秦岭南亚带硅灰泥岩型金矿床的成矿条件及热液隐爆成因  

The metallogenic conditions of the gold deposits of siliceous mudstone type in south subzone of western Qinling and the genesis of concealed hydrothermal eruption

作　　者：周德安[1] 钱发荣 漆富成[1] 尹金双[1] 张淑苓 王驹[1] 黄树桃[1] 

机构地区：[1]核工业北京地质研究院

出　　处：《黄金》1995年第2期5-12,共8页Gold

摘　　要：本文通过对西秦岭南亚带硅灰泥岩型金矿床的分析研究，首次提出金矿床的热液隐爆成因，并建立了相应的成矿模式。Through analysis of the gold deposits of siliceous mudstone type in south subzone of western Qinling,this paper firstly pointed out the genesis of concealed hydrothermal eruption and established their metallogenic model.

关 键 词：硅灰泥岩型 金矿床 热液隐爆成因 成矿模式 成因 

分 类 号：P618.510.1[天文地球—矿床学]