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甘肃枣子沟金矿围岩蚀变特征及其与金矿化的关系
引用本文:代文军,陈耀宇,刘春先,刘东晓,马小云. 甘肃枣子沟金矿围岩蚀变特征及其与金矿化的关系[J]. 甘肃地质, 2011, 0(3): 31-36
作者姓名:代文军  陈耀宇  刘春先  刘东晓  马小云
作者单位:[1]甘肃省地矿局第三地勘院,甘肃兰州730050 [2]甘肃省国土资源厅,甘肃兰州730000
摘    要:枣子沟金矿位于新堡—力士山复背斜南翼之合作—岷县区域断裂带南侧,是西秦岭西段近些年发现并勘查的大型金矿床之一。其围岩蚀变发育,类型多样。发育有区域地层变质期的面型热液蚀变作用和构造热作用的线型热液蚀变作用两类主要蚀变,其中线型蚀变中的硅化、黄铁矿化、毒砂化及辉锑矿化等蚀变与金矿化关系密切,可作为夏河—合作金矿富集区找矿...

关 键 词:金矿床  围岩蚀变  蚀变与矿化  枣子沟  甘肃

Wallrock Alteration and Gold Mineralization in Zaozigou Gold Mine of Gansu Province
DAI Wen-jun,CHEN Yao-yu,LIU Chun-xian,LIU Dong-xiao and MA Xiao-yun. Wallrock Alteration and Gold Mineralization in Zaozigou Gold Mine of Gansu Province[J]. Acta Geologica Gansu, 2011, 0(3): 31-36
Authors:DAI Wen-jun  CHEN Yao-yu  LIU Chun-xian  LIU Dong-xiao  MA Xiao-yun
Affiliation:1.No.3 Geology and Mineral Exploration Team,Gansu Provincial Bureau of Geology and Mineral Exploration and Development,Lanzhou 730050,China; 2.Department of Land and Resources in Gansu Province,Lanzhou 730000,China)
Abstract:Zaozigou gold mine is situated the south side of Hezuo-Minxian Fault zone which is the south limb of Xinbao-Lishishan anticlinorium.It is a large scale gold deposit discovered in the west section west Qinling in rescent years.Among the various type of wallrock alteration,the most important types are these two: planar hydrothermal alteration occurred during regional metamorphic period,and linear hydrothermal alteration caused by structural heat activities.Silicification,pytization,arsenpyritization and animonitization of linear alteration were close to gold mineralization.
Keywords:alteration  gold mineralization  Zaozigou gold deposit  Gansu
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