| 云南富源县富盛铅锌矿地质特征及成因浅析 |
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| 引用本文： | 洪明春,朱勋帅,李华明.云南富源县富盛铅锌矿地质特征及成因浅析[J].世界有色金属,2020(4):109-109,111. |
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| 作者姓名： | 洪明春 朱勋帅 李华明 |
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| 作者单位： | 云南源浩矿业有限公司,云南昆明 650051;云南源浩矿业有限公司,云南昆明 650051;云南源浩矿业有限公司,云南昆明 650051 |
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| 摘 要： | 通过对研究区地质特征及矿物富集特征进行分析,认为富盛铅锌矿矿区位于新君台矿段,矿体主要赋存于二叠系茅口组第二段的大理石化白云岩中,矿体呈似层状、透镜状、脉状产出,矿体由北西向南东埋深逐渐增大,矿体产状与大理岩化白云岩岩一致。矿体多分布于北东、北西、南北多组构造交切处,特别是北西、南北两组构造结点附近矿体较富厚特征。
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| 关 键 词： | 铅锌矿 地质特征 成因 |
Geological characteristics and genesis of fusheng lead-zinc deposit in fuyuan county,yunnan province |
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| HONG Ming-chun,ZHU Xun-shuai,LI Hua-ming.Geological characteristics and genesis of fusheng lead-zinc deposit in fuyuan county,yunnan province[J].World Nonferrous Metals,2020(4):109-109,111. |
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| Authors: | HONG Ming-chun ZHU Xun-shuai LI Hua-ming |
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| Affiliation: | (Yunnan yuanhao mining Co.Ltd.,Kunming 650051,China) |
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| Abstract: | Based on the geological characteristics and mineral enrichment characteristics in the study area were analyzed,and the thought rich sheng lead-zinc mine mining area is located in the new king ore block,the ore bodies mainly occur in the Permian MAO petrochemical dolomite marble of the second paragraph,ore body is like a layered,lenticular,vein output,orebody from north west to south east buried depth increases gradually,the orebody occurrence and Dali lithification dolomite rock.The ore bodies are mostly distributed at the intersection of the north east,north west and north and south tectonic groups. |
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| Keywords: | lead-zinc ore geological characteristics genesis |
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