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    李建荣, 孙华, 刘伟东, 侯冬红, 赵建新. 2020. 山西省垣曲县幅1∶50 000地质图数据库[J].中国地质,47(S1):135−145. DOI: 10.12029/gc2020Z113
    引用本文: 李建荣, 孙华, 刘伟东, 侯冬红, 赵建新. 2020. 山西省垣曲县幅1∶50 000地质图数据库[J].中国地质,47(S1):135−145. DOI: 10.12029/gc2020Z113
    孙华; 侯冬红; 刘伟东; 赵建新; 李建荣. 山西省垣曲县幅 1∶50 000 地质图数据库 (V1). 山西省地质调查院; 山西省地质勘查局214地质队[创建机构], 2016. 全国地质资料馆[传播机构], 2020-06-30. 10.35080/data.A.2020.P13; http://dcc.cgs.gov.cn/cn//geologicalData/details/doi/10.35080/data.A.2020.P13. DOI: 10.12029/gc2020Z113
    Citation: 孙华; 侯冬红; 刘伟东; 赵建新; 李建荣. 山西省垣曲县幅 1∶50 000 地质图数据库 (V1). 山西省地质调查院; 山西省地质勘查局214地质队[创建机构], 2016. 全国地质资料馆[传播机构], 2020-06-30. 10.35080/data.A.2020.P13; http://dcc.cgs.gov.cn/cn//geologicalData/details/doi/10.35080/data.A.2020.P13. DOI: 10.12029/gc2020Z113

    山西省垣曲县幅1∶50 000地质图数据库

    1∶50 000 Geological Map Database of Yuanqu Map-sheet, Shanxi Province

    • 摘要: 山西省垣曲县幅(I49E005015)1∶50 000地质图数据库是根据中国地质调查局地质调查工作和地质行业的统一标准及要求,在充分利用该区1∶200 000、1∶250 000等区域地质矿产调查成果资料的基础上,通过采用数字填图系统进行野外地质填图形成的。野外共采集岩石化学分析样品54件,同位素测年样品7件。通过本数据库的建立,对中条山地区“涑水杂岩”进行了解体,查明了该区变质基底的物质组成及构造轮廓;对古元古界进行了重新厘定划分,提出中条山地区古元古界新的划分方案;对中元古界熊耳群进行了“火山构造−岩性岩相−火山地层”三重填图及同位素测年,限定了该区中元古界的底界年龄;系统总结了该区变质岩建造特征;提出中条山地区古元古代3期构造叠加样式,对中条山核心铜矿区胡–篦型铜矿的成矿规律、构造控矿的研究有重要指导意义。

       

      Abstract: The 1∶50 000 geological map database of Yuanqu map-sheet (I49E005015), Shanxi Province was developed in accordance with the standards and requirements of geological surveys proposed by the China Geological Survey and the unified standards and requirements applicable to the geological industry, for which the achievements obtained from previous 1∶200 000 and 1∶250 000-scale regional geological surveys were fully utilized. Meanwhile, the Digital Geological Survey System (DGSS) was adopted for geological field mapping. A total of 54 samples for petrochemical analysis and seven samples for isotope dating were collected in the field. The following achievements were obtained by establishing the Database. The material composition of the metamorphic basement in Zhongtiao Mountain area and the tectonic framework of the area were ascertained by breaking up the Sushui complex in the area. The Paleoproterozoic boundary of Zhongtiao Mountain was redetermined and a new division scheme of the boundary was put forward. The volcanic structures, lithology and lithofacies, and volcanic strata of the Mesoproterozoic Xiong’er Group were mapped, and isotopic dating was conducted for the group. As a result, the age of Mesoproterozoic lower boundary of Zhongtiao Mountain was restricted. Furthermore, the characteristics of metamorphic rock formations were systematically summarized, and three stages of tectonic superimposition patterns of the Paleoproterozoic in Zhongtiao Mountain were proposed. All these will provide important guidance for the research on metallogenic rules and controlling structures of the Hu-Bi type copper deposits in the core Cu mining area in Zhongtiao Mountain.

       

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