中山沟金矿成矿作用研究  

Study on Mineralization of Zhongshangou Gold Deposi

作　　者：郑宏伟[1] 王丰翔[1] 宋鹏[1] 王国晨[1] 

机构地区：[1]石家庄经济学院,河北石家庄050031

出　　处：《科技视界》2013年第19期177-177,204,共2页Science & Technology Vision

摘　　要：中山沟金矿位于张宣幔枝构造西缘,是张宣幔枝构造演化过程中形成的石英脉型金矿。本文以幔枝构造理论为指导,通过野外调查,室内综合分析,对其成矿作用进行分析,认为其东西两侧的构造蚀变破碎带及深部仍具有很大找矿潜力。Zhongshangou gold deposit located in the west of Zhang-Xuan mantle branch,is quartz vein type gold formed in the evolution of mantle branch. Using Mantle branch theory as a guide, through field survey and indoor comprehensive analysis, analyze its mineralization. This paper holds that the peripheral and deep of Zhongshangou gold deposit still have a great prospecting potential.

关 键 词：幔枝构造 成矿作用 控矿构造 张宣地区 中山沟金矿 

分 类 号：P618.510.5[天文地球—矿床学]