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敦化市松江河金矿地质特征简述
引用本文:刘东伟,梁世福,于政涛,姜福旭.敦化市松江河金矿地质特征简述[J].吉林地质,2009,28(3):26-28.
作者姓名:刘东伟  梁世福  于政涛  姜福旭
作者单位:1. 吉林省地质调查院,吉林,长春,130061
2. 吉林省绿色食品办公室,吉林,长春,130062
摘    要:松江河金矿位于夹皮沟—海沟金成矿带的中部,矿床产于色洛河岩群中,矿体受近南北向构造带控制,矿石类型为蚀变岩和石英脉两种,矿床成因类型为构造蚀变岩型。

关 键 词:矿床特征  金矿  松江河

Geologic features of the Songjianghe Au deposit Dunhua City
LIU Dong-wei,LIANG Shi-fu,YU Zheng-tao,JIANG Fu-xu.Geologic features of the Songjianghe Au deposit Dunhua City[J].Jilin Geology,2009,28(3):26-28.
Authors:LIU Dong-wei  LIANG Shi-fu  YU Zheng-tao  JIANG Fu-xu
Institution:LIU Dong-wei, LIANG Shi-fu ,YU Zheng-tao ,JIANG Fu-xu( 1. Institute of Geologic Survey of Jilin Province, Changchun 130061,Jilin, China 2. The Green Food Office of Jilin Province. Changchun 130062,Jilin, China)
Abstract:Songjianghe Au deposit is located in the middle part of the Au ore-forming belt of the Jiapigou-Haigou,The deposit occurs in the Seluohe Group.The orebody is controlled by approximately SN structure.Ore style belongs to altered rock and quartz vein type,the genetic type belongs to altered rock of structure.
Keywords:deposit character  Au depsit Songjianghe
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