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.
出处
《吉林地质》
2012年第1期49-54,共6页
Jilin Geology
关键词
矿床特征
铅、锌、钼多金属
翠干公路岭上
deposit features
lead
zinc
molybdenum polymetallic deposit
mountain of Cuigan highway
作者简介
潘建（1970-），男，内蒙古赤峰人，吉林省区域地质矿产调查所工程师．
