首页|云南华坪基度大理岩矿床地质特征及成因分析

云南华坪基度大理岩矿床地质特征及成因分析

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基度大理岩矿床位于扬子陆块盐源—丽江被动陆源北部,构造不甚发育,岩浆活动强烈,变质作用微弱.通过对区域地质背景、矿区地质特征的分析,厘定了矿床地质特征及成因.矿区共圈定2个大理岩矿体,赋矿层位为二叠中统阳新组,矿体规模大、厚度稳定,发育瓷白大理石、米黄大理石及银灰大理石.结合矿床成矿地质条件、矿石矿物特征等,认为矿床属海相化学、生物沉积型大理岩矿床,含矿层北东延伸方向具有较大的找矿潜力.
Geological Characteristics and Genesis Analysis of Jidu Marble Deposit in Huaping County,Yunnan Province
The Jidu marble deposit is located in the northern part of the Yanyuan-Lijiang passive con-tinental source of the Yangtze block.The structure is not well developed,the magmatic activity is strong,and the metamorphism is weak.Through the analysis of regional geological background and geological charac-teristics of the mining area,the geological characteristics and genesis of the deposit are determined.Two mar-ble ore bodies are delineated in the mining area.The ore-bearing strata are the Yangxin Formation of the Middle Permian.The ore body is large in scale and stable in thickness.Porcelain white marble,beige mar-ble and silver gray marble are developed.Combined with the metallogenic geological conditions and ore min-eral characteristics of the deposit,it is considered that the deposit belongs to marine chemical and biological sedimentary marble deposit,and the ore-bearing layer has great prospecting potential in the northeast exten-sion direction.

deposit geologyore genesismarble mineprospecting perspective

杨继春

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中国建筑材料工业地质勘查中心云南总队

矿床地质 矿床成因 大理岩矿 找矿远景

2024

现代矿业
中钢集团马鞍山矿山研究院有限公司

现代矿业

影响因子:0.33
ISSN:1674-6082
年,卷(期):2024.40(4)
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