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    构造体制转换与流体多层循环成矿动力学

    邓军 杨立强 孙忠实 彭润民 陈学明 杜子图

    邓军, 杨立强, 孙忠实, 彭润民, 陈学明, 杜子图, 2000. 构造体制转换与流体多层循环成矿动力学. 地球科学, 25(4): 397-403.
    引用本文: 邓军, 杨立强, 孙忠实, 彭润民, 陈学明, 杜子图, 2000. 构造体制转换与流体多层循环成矿动力学. 地球科学, 25(4): 397-403.
    DENG Jun, YANG Liqiang, SUN Zhongshi, PENG Runmin, CHEN Xueming, DU Zitu, 2000. ORE-FORMING DYNAMICS OF TECTONIC REGIME TRANSFORMATION AND MULTI-LAYER FLUID CIRCULATION. Earth Science, 25(4): 397-403.
    Citation: DENG Jun, YANG Liqiang, SUN Zhongshi, PENG Runmin, CHEN Xueming, DU Zitu, 2000. ORE-FORMING DYNAMICS OF TECTONIC REGIME TRANSFORMATION AND MULTI-LAYER FLUID CIRCULATION. Earth Science, 25(4): 397-403.

    构造体制转换与流体多层循环成矿动力学

    基金项目: 

    国家重点基础研究发展规划项目 G1999043206

    国土资源部“百名跨世纪科技人才培养计划”基金 9808

    国家攀登计划项目 95-预-25

    国家攀登计划项目 95-预-39

    ;国土资源部“九五”重点基础项目 9501103

    详细信息
      作者简介:

      邓军,男,1958年生,教授,博士生导师,构造地质学和矿床学专业,主要从事区域构造、成矿流体及成矿动力学的教学和科研工作

    • 中图分类号: P611.5; P542

    ORE-FORMING DYNAMICS OF TECTONIC REGIME TRANSFORMATION AND MULTI-LAYER FLUID CIRCULATION

    • 摘要: 基于成矿系统动力学研究进展的综合分析, 认为构造体制转换与流体多层循环成矿动力学研究是地球科学跨世纪的重要前沿领域之一, 进而提出这一领域的研究主题和关键问题、研究思路及方法, 阐释其重要意义, 指出构造体制转换与流体多层循环成矿动力学研究以构造演化、流体活动及区域地球化学和地球物理不均一性为基础, 通过变形-流动高温高压实验及计算机数值模拟再现成矿作用过程和机理, 解析构造体制转换与流体多层循环成矿动力学特征, 揭示成矿界面时-空演化规律, 建立成矿系统物质和能量交换-反馈耦合成矿的定量模型.这是深化矿床成因认识的重要基础和实现科学找矿的有效途径, 对地球系统科学和大陆动力学的研究也具有重要意义.

       

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