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吉林省松树川银矿床地质特征及找矿方向
引用本文:孙云飚,周树亮,孙雪峰,冯修云. 吉林省松树川银矿床地质特征及找矿方向[J]. 吉林地质, 2010, 29(4): 27-31
作者姓名:孙云飚  周树亮  孙雪峰  冯修云
作者单位:吉林省有色金属地质勘查局六O七队,吉林吉林市132105
摘    要:松树川银矿床产于燕山期闪长玢岩接触部闪长玢岩体内,矿化类型为硅化蚀变破碎带类型,矿体受区内的北东向—北西向断裂及裂隙构造控制,矿床为受次火山作用控制的中—低温热液型独立的银矿床,矿床工业类型为脉状银矿床。

关 键 词:找矿方向  地质特征  松树川银矿  吉林省

Geologic features and prospecting direction of Songshuchuan silver deposit,Jilin Province
SUN Yun-biao,ZHOU Shu-liang,SUN Xue-feng,FENG Xiu-yun. Geologic features and prospecting direction of Songshuchuan silver deposit,Jilin Province[J]. Jilin Geology, 2010, 29(4): 27-31
Authors:SUN Yun-biao  ZHOU Shu-liang  SUN Xue-feng  FENG Xiu-yun
Affiliation:Team 607,Bureau of Nonferrous Metals Geologic Exploration of Jilin Province,Jilin 132105,Jilin,China
Abstract:The Songshuchuan silver deposit occurs in Yanshanian diorite porphyrite which belongs the silicated fracture alteration zone in mineralization,orebody in the study area is controlled by NE–NW trending faults and fracture structures;ore deposit is controlled by the subvolcanism,which belongs to low-to-moderate hydrothermal independent vein silver deposits.
Keywords:prospecting direction  geologic features  silver deposit of Songshuchuan  Jilin Province
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