金厂峪金矿床成矿模式探讨  

Discussion on metallogenic model of Jinchangyu gold deposit

作　　者：任广智[1] 张友刚 

机构地区：[1]中国黄金集团公司,北京100011 [2]金厂峪金矿,河北迁西064300

出　　处：《中国矿山工程》2010年第5期48-50,共3页China Mine Engineering

摘　　要：金厂峪金矿受控于太古界地层、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—重熔中温热液石英脉型金矿床。Jinchangyu gold deposit was controlled by Archean group strata,ductile shear belt and Qingshankou rock mass inYanshan.The ore-forming process was multi-period and multi-stage.The deposit genesis belongs to metamorphogenic remelting mesother mal quartz gold-bearing deposit.

关 键 词：韧性剪切带 成矿模式 探讨 

分 类 号：P618.51[天文地球—矿床学]