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。
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.
出处
《吉林地质》
2009年第3期26-28,共3页
Jilin Geology
关键词
矿床特征
金矿
松江河
deposit character, Au depsit Songjianghe
