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。
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.
出处
《吉林地质》
2010年第4期27-31,共5页
Jilin Geology
关键词
找矿方向
地质特征
松树川银矿
吉林省
prospecting direction
geologic features
silver deposit of Songshuchuan
Jilin Province
