王肖,王陆超,张凯,王亮,赵盛博,洪连明.苏北超高压变质带新集石墨矿地质特征及成因分析[J].地质找矿论丛,2023,38(1):37-43
苏北超高压变质带新集石墨矿地质特征及成因分析
Geological characteristics and Genesis of Xinji graphite deposit in ultrahigh pressure metamorphic belt of northern Jiangsu province
投稿时间:2022-05-10  
DOI:10.6053/j.issn.1001-1412.2023.01.005
中文关键词:  新集石墨矿  地质特征  碳质来源  苏北地区
英文关键词:Xinji graphite deposit  geological characteristics  carbon source  northern Jiangsu province
基金项目:江苏省地质矿产勘查局地勘基金项目(编号:苏地矿发〔2019〕104号)资助。
作者单位
王肖 江苏省地质矿产局第六地质大队, 江苏 连云港 222023 
王陆超 江苏省地质矿产局第六地质大队, 江苏 连云港 222023 
张凯 江苏省地质矿产局第六地质大队, 江苏 连云港 222023 
王亮 江苏省地质矿产局第六地质大队, 江苏 连云港 222023 
赵盛博 江苏省地质矿产局第六地质大队, 江苏 连云港 222023 
洪连明 江苏省地质矿产局第六地质大队, 江苏 连云港 222023 
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中文摘要:
      苏北超高压变质带新集石墨矿矿体赋存于东海群班庄组,矿体受地层控制明显。本文通过研究石墨矿体地质特征,分析石墨矿石主要成分并与扬子陆块各类沉积岩对比,结合区域碳同位素判别物源。结果表明,新集石墨矿石主要为石墨石英片岩型石墨矿石;成矿原岩为碳质泥岩,但与一般碳质泥岩相比,CaO、MgO的富集程度更高,是成分较为特殊的碳质泥岩;矿石中碳同位素δ13C)=-31.2×10-3~-22.3×10-3,围岩大理岩δ13C)=-0.8×10-3~0.2×10-3,石墨与大理岩的碳同位素分布区间完全不同,二者没有重叠区,说明它们的碳质具有不同来源,石墨碳来源于有机沉积物。
英文摘要:
      Xinji graphite deposit occurs in Banzhuang formation of Donghai Group in ultrahigh pressure metamorphic belt of northern Jiangsu province. Ore bodies are obviously controlled by strata. This paper deals with geological characteristics of the deposit, analysis of constituents of the graphite ore and comparison of the strata with each sedimentary rocks in Yangtze continental block to discriminate material source of the strata with help of regional isotropic data. The ore is mainly composed of graphite-quartz schist type ore. The original rock of the strata is carbonaceous mudstone. Compared with ordinary mudstone the original rock is richer in CaO, MgO. δ13C of the graphite ore is -31.2×10-3~22.3×10-3, δ13C of the host marble -0.8×10-3~0.2×10-3 distributing in different ranges without overprinting. Such phenomenon suggests that their C comes from different source. C of the graphite ore comes from organic sediments.
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