摘要
西林河银及多金属矿床属于剪切带型矿床 ,矿区构造活动、成矿作用、围岩蚀变是同时进行、相互作用的。矿体严格受构造裂隙控制 。
Following the Shanmen silver deposit, Siping, Jilin Province, the Xilin silver and polymetallic ore deposit is an other important discovery. The ore deposit belongs to shear belt type, tectonic activity, ore-forming process and wall-rock alteration in the mining area are simultaneous and interaction. The ore body is strictly controlled by the fractures and without relation with the lithologic character.
出处
《吉林地质》
2001年第1期12-18,共7页
Jilin Geology