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江苏新沂城岗石墨矿地质特征及找矿标志

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城岗石墨矿位于华北板块东南缘,处在郯庐断裂带之间.城岗石墨矿赋存于新太古代—古元古代城岗岩群中部,呈层状、似层状产出,矿体规模较大.矿石自然类型为片麻岩型石墨矿,矿石质量良好.矿床成因为区域变质型石墨矿,系含有机质的钙质碎屑岩及碳酸盐岩经后期区域变质作用形成.城岗石墨矿找矿标志较明显,与石墨矿化密切相关的岩性主要为含石墨透辉(或透闪)斜长片麻岩、透辉斜长片麻岩、大理岩等.
Geological Characteristics and Prospecting Indicators of The Chenggang Graphite Deposit in Xinyi,Jiangsu
The Chenggang graphite mine is located on the southeastern edge of the North China Plate,between the Tanlufault zone.The Chenggang graphite deposit is located in the middle of the Neoarchean Paleoproterozoic Chenggang rock group,and is produced in a layered or quasi layered manner.The ore body is relatively large in scale.The natural type of ore is gneiss type graphite ore,with good ore quality.The formation of the ore deposit is due to regional metamorphic graphite deposits,which are composed of calcareous clastic rocks and carbonate rocks containing organic matter formed through later regional metamorphism.The prospecting indicators for the Chenggang graphite deposit are obvious,and the lithology closely related to graphite mineralization is mainly graphite containing diopside(or tremolite)plagioclase gneiss,diopside plagioclase gneiss,marble,etc.

graphite depositChenggangNorthern Jiangsuprospecting indicator

姚维军、张洋洋、石林、刘峰、沈瑞、张珣

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江苏省地质勘查技术院,江苏 南京 210049

石墨矿 城岗 苏北 找矿标志

江苏省自然资源发展专项江苏省自然资源发展专项江苏省自然资源发展专项

苏财资环[2021]46号苏财资环[2022]27号苏财资环[2023]30号

2024

中国非金属矿工业导刊
中国中材集团有限公司 中国建筑材料工业地质勘查中心 中国非金属矿工业协会

中国非金属矿工业导刊

CSTPCD
影响因子:0.39
ISSN:1007-9386
年,卷(期):2024.(3)