金厂峪金矿床成矿地质特征及成矿模式  

The geological feature of the metallization of Jinchangyu gold deposit and its metallogenic model

作　　者：水兰素[1] 常全明[1] 

机构地区：[1]河北理工学院

出　　处：《黄金》2000年第11期6-8,共3页Gold

摘　　要：金厂峪金矿床受控于太古界地层、韧性剪切带和燕山期青山口岩体 ,成矿作用具有多期多阶段的特点 ,矿床成因属变质—重熔岩浆热液复生金矿床。Jinchangyu gold ore deposit is controlled by the Archean Group stratum ,ductile shear zones and the Qing shankou rock mass of Yanshan stage.The mineralization is of the characteristics of poly epoches and poly stage.The deposit genesis belongs to the metamorphism-anatectic magma hydrothermal reproduction gold deposit

关 键 词：韧性剪切带 成矿模式 金矿床 成矿地质特征 

分 类 号：P618.51[天文地球—矿床学]