摘要
金山矿区位于新疆天山西段,隶属伊宁县管辖范围,矿区内分布有三个成矿区,分别为马依托拜成矿区和京希成矿区以及伊尔曼得成矿区等。金山矿区主要为山岭地形,分布于河间区域,呈南北向展布。地质构造仅见一个背斜构造,侵入岩不发育。气候特点为大陆性温带气候,矿区水文地质与地下水埋深存在很大关系,主要地下水类型分为松散岩类孔隙水,以基岩裂隙水与岩溶水等。
Xinjiang Jinshan mine is located in the Western Tianshan,under the Yining County jurisdiction,area distribution has three metallogenic zone,respectively,relying on mining and horse worship Jingxi yelmend metallogenic metallogenic area and etc..Jinshan mining area is mainly distributed in the mountainous terrain,river area,north-south trending.The geological structure only one anticline,the intrusive rocks are not developed.The climate is characterized by continental temperate climate.There is a great relationship between the hydrogeology and groundwater depth.
出处
《世界有色金属》
2017年第3期110-110,112,共2页
World Nonferrous Metals
关键词
金山矿区
水文地质
Jinshan mining area hydrogeology