牙克石市翠干公路岭上铅锌钼多金属矿床地质特征简述  

Geological features of Cuigan mountain lead-zinc polymetallic deposit,Yakeshi City,Inner Mongolia

作　　者：潘建[1] 常立海 王嵩莉[3] 代丽霞[1] 

机构地区：[1]吉林省区域地质矿产调查所,吉林长春130022 [2]黑龙江省桩基础工程公司,黑龙江哈尔滨1500363 [3]吉林大学应用技术学院,吉林长春130012

出　　处：《吉林地质》2012年第1期49-54,共6页Jilin Geology

摘　　要：该矿床位于阿尔山—博克图—鄂伦春成矿带的中南部,产于晚侏罗世玛尼吐组之中,矿体受北西向次级构造控制,成因类型为斑岩型及破碎带蚀变岩型。The ore deposit is located in the mid-southern part of the Arshan-Boketu-Elunchun metallogenic belt,occurred in the late Jurassic Marnitu Group , ore bodies were controlled by WN secondary structure, It belongs to porphyry and fracture altered rock type in genesis.

关 键 词：矿床特征 铅、锌、钼多金属 翠干公路岭上 

分 类 号：P618.42[天文地球—矿床学] P618.43[天文地球—地质学]