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现代矿业 ›› 2016, Vol. 32 ›› Issue (09): 145-148.

• 地质·测量 • 上一篇    下一篇

云南麻栗坡县龙沟锰矿地质特征及成因

赵民,高永宝,贺永康,陈登辉,燕洲泉,李侃,隋清霖   

  1. 中国地质调查局西安地质调查中心
  • 出版日期:2016-09-20 发布日期:2016-11-14

Geological Characteristics and Genesis of Longgou Manganese Deposit in Malipo County,Yunnan Province

Zhao Min,Gao Yongbao,He Yongkang,Chen Denghui,Yan Zhouquan,Li Kan,Sui Qinglin   

  1. Xi'an Center of Geological Survey,China Geological Survey
  • Online:2016-09-20 Published:2016-11-14

摘要: 龙沟锰矿床位于滇东南优质富锰矿产区斗南成矿带,矿体赋存于中三叠统法郎组(T2f)地层中,呈似层状、透镜状产出,与围岩产状基本一致,赋矿岩性为泥岩、粉砂质泥岩夹含砾砂岩、细砂岩和硅质岩,沉积环境为滨海—浅海相。结合区内地质工作成果,在分析区域地质背景、矿区地质特征、矿床地质特征的基础上,对矿床锰质来源、沉积环境进行了讨论,认为该矿床成因类型属于遭受后期次生氧化改造的滨海—浅海相沉积锰矿床。上述分析对于区内进一步开展锰矿找矿工作有一定的参考价值。

关键词: 锰矿床, 区域地质背景, 地质特征, 沉积环境, 矿床成因

Abstract: Longgou manganese deposit is located in Dounan metallogenic belt,that is the high-quality manganese ore belt in the southeast Yuannan province.The ore-bodies are located in the middle Triassic Falang formation,they are exposed with layered and lenticular shapes,which is similar with the occurrence of surrounding rock.The ore-bearing rocks are mudstone,silty mudstone interbedded with conglomeratic sandstone,fine sandstone and siliceous rocks.The sedimentary environment is littoral-neritic facies.Based on the geological working results of the mining area,the regional geological background,geological characteristics of the mining area,geological characteristics of the deposits are analyzed,and the source of manganese,sedimentary environment are discussed,the results show that the genetic type of the deposit is the littoral-neritic facies manganese deposit that is suffered the secondary oxidation transformation.The above analysis result can provide some reference for the further prospecting work of manganese deposit in the mining area.

Key words: Manganese deposit, Regional geological background, Geological characteristics, Sedimentary environment, Deposit genesis