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| 牙克石市翠干公路岭上铅锌钼多金属矿床地质特征简述 | |
| 引用本文： | 潘建,常立海,王嵩莉,代丽霞.牙克石市翠干公路岭上铅锌钼多金属矿床地质特征简述[J].吉林地质,2012,31(1):49-54. |
| 作者姓名： | 潘建 常立海 王嵩莉 代丽霞 |
| 作者单位： | 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,150036 3. 音林大学应用技术学院,吉林长春,130012 |
| 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。 |
| 关 键 词： | 矿床特征 铅、锌、钼多金属 翠干公路岭上 |
Geological features of Cuigan mountain lead-zinc polymetallic deposit,Yakeshi City,Inner Mongolia |
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| PAN Jian,CHANG Li-hai,WANG Song-li,DAI Li-xia.Geological features of Cuigan mountain lead-zinc polymetallic deposit,Yakeshi City,Inner Mongolia[J].Jilin Geology,2012,31(1):49-54. | |
| Authors: | PAN Jian CHANG Li-hai WANG Song-li DAI Li-xia |
| Institution: | 1.Regional Geologic Survey of Jilin Province, Changchun 130022, Jilin, China; 2.Pile Foundation Engineering Company of Heilongjiang Province, Harbin 150036, Heilongjiang, China; 3.Institute of Applied Technology, Jilin University, Changchun 130012, Jilin, China |
| Abstract: | 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. |
| Keywords: | deposit features lead zinc molybdenum polymetallic deposit mountain of Cuigan highway |
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