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    中国东部中、新生代软流圈上涌与构造-岩浆-矿集区

    邢集善 杨巍然 邢作云 刘建华

    邢集善, 杨巍然, 邢作云, 刘建华, 2019. 中国东部中、新生代软流圈上涌与构造-岩浆-矿集区. 地球科学, 44(5): 1570-1583. doi: 10.3799/dqkx.2019.976
    引用本文: 邢集善, 杨巍然, 邢作云, 刘建华, 2019. 中国东部中、新生代软流圈上涌与构造-岩浆-矿集区. 地球科学, 44(5): 1570-1583. doi: 10.3799/dqkx.2019.976
    Xing Jishan, Yang Weiran, Xing Zuoyun, Liu Jianhua, 2019. Meso-Cenozoic Asthenosphere Upwelling of Eastern China and Its Impacts on Structure-Magma-Mineralization Concentration Region. Earth Science, 44(5): 1570-1583. doi: 10.3799/dqkx.2019.976
    Citation: Xing Jishan, Yang Weiran, Xing Zuoyun, Liu Jianhua, 2019. Meso-Cenozoic Asthenosphere Upwelling of Eastern China and Its Impacts on Structure-Magma-Mineralization Concentration Region. Earth Science, 44(5): 1570-1583. doi: 10.3799/dqkx.2019.976

    中国东部中、新生代软流圈上涌与构造-岩浆-矿集区

    doi: 10.3799/dqkx.2019.976
    基金项目: 

    中国地质调查局项目 1212010733802

    中国地质调查局项目 12120113012500

    中国地质调查局项目 1212011220529

    详细信息
      作者简介:

      邢集善(1936-), 男, 教授级高工, 主要从事深部地球物理及构造地质研究

    • 中图分类号: P31

    Meso-Cenozoic Asthenosphere Upwelling of Eastern China and Its Impacts on Structure-Magma-Mineralization Concentration Region

    • 摘要: 以深部地球物理资料为基础, 结合大地构造环境、岩浆岩同位素示踪及矿产资源分布规律, 加以综合分析.通过热力学计算可知, 中国东部近2亿年来的上地幔岩石圈/软流圈构造可以存留至今, 且能区分出中、新生代.软流圈上涌与矿集区:(1)中生代金属矿:(a)克拉通区, 软流圈沿柱身上涌, 其柱头上方形成幔壳混熔花岗质岩及相应Au、Cu、Mo、Pb-Zn等矿集区, 并于柱身与岩石圈块体陡接触带, 形成中基性杂岩及相应富Fe矿集区; (b)褶皱带区, 在软流圈上涌柱上方形成近幔源型花岗质岩, 相应为Cu、Au、Pb-Zn、Mo、Ag矿集区; (c)南岭带, 软流圈层在适当深度、热量充足、较大范围内"平卧", 因热传导而致使地壳内物质部分重熔, 形成壳源型花岗质岩及相应的W、Sn、稀有元素矿集区; (2)新生代油气田:(a)与太平洋板块俯冲有关的软流圈上涌, 其上方出露玄武岩, 形成较大型油田; (b)与裂陷盆地有关的软流圈上涌, 其上方形成大型油田, 也有中小型油田.软流圈上涌与大地构造:中生代J-K时期, 通过构造力特征等的综合分析, 阐明燕山运动的根源及其影响; 新生代侧重剖析大陆裂谷相关特征.总之, 软流圈上涌是岩石圈减薄, 以及中、新生代构造-岩浆-矿集区形成的根源.

       

    • 图  1  中国东部(大陆)MOHO面深度图

      邢集善等(2007)修编

      Fig.  1.  Sketch of MOHO depth of eastern China (mainland)

      图  2  中国东部(大陆)岩石圈/软流圈构造图

      邢集善等(2009)修编

      Fig.  2.  Structure of lithosphere/asthenosphere of eastern China (mainland)

      图  3  华北地震层折成象115°E南北向剖面

      邢作云等(2006a, 2006b)修编

      Fig.  3.  Seismic tomographic image along 115°E S-N section of North China

      图  4  华南地震层析成像HW9东西向剖面

      邢集善等(2009)修编

      Fig.  4.  Seismic tomographic image along HW9 E-W section of South China

      图  5  华南地震层析成像HW5东西向剖面

      邢集善等(2009)修编

      Fig.  5.  Seismic tomographic image along HW5 E-W section of South China

      图  6  华北地震层析成像沿38.7°N东西向剖面

      邢作云等(2006a, 2000b)修编

      Fig.  6.  Seismic tomographic image along 38.7°N E-W section of North China

      图  7  东北地区东乌旗-大兴安岭(南)-丹东大地电磁测深剖面

      据国家地震局(1992)修编

      Fig.  7.  Magnetotelluric sounding profile of Dongwuqi-Daxing'anling (south)-Dandong in Northeast China

      图  8  临汾断陷电性结构剖面与地震图

      邢作云等(2005)修编

      Fig.  8.  Faulted electricity structure section of Linfen subsidence

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    • 收稿日期:  2019-02-20
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