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盆山耦合与沉积盆地成因

王清晨 李忠

王清晨, 李忠. 盆山耦合与沉积盆地成因[J]. 沉积学报, 2003, 21(1): 24-30.
引用本文: 王清晨, 李忠. 盆山耦合与沉积盆地成因[J]. 沉积学报, 2003, 21(1): 24-30.
WANG Qing-chen, LI Zhong. Basin-Orogen Coupling and Origin of Sedimentary Basins[J]. Acta Sedimentologica Sinica, 2003, 21(1): 24-30.
Citation: WANG Qing-chen, LI Zhong. Basin-Orogen Coupling and Origin of Sedimentary Basins[J]. Acta Sedimentologica Sinica, 2003, 21(1): 24-30.

盆山耦合与沉积盆地成因

基金项目: 国家重点基础研究发展规划 ( 973)项目 G19990 4330 3课题资助
详细信息
  • 中图分类号: P512.2

Basin-Orogen Coupling and Origin of Sedimentary Basins

  • 摘要: 我国的沉积盆地成因研究主要遵循盆山耦合的研究思路进行 ,关注重点为盆山体系的构造、沉积和深部结构上的耦合现象。构造耦合研究是指盆山结合带的统一变形特征 ,沉积耦合研究是通过沉积响应去重塑盆山耦合过程及相邻造山带的演化过程 ,深部结构耦合的重点是研究盆山体系在岩石圈尺度的动力学统一性。国际上相应领域的研究重点为岩石圈深部过程与近地表构造过程的耦合。国内外研究既有相同之处 ,又有差异之处。建议在未来的沉积盆地成因研究中更加开阔思路 ,采用天然实验室的工作模式 ,进行多学科综合研究。
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出版历程
  • 收稿日期:  2002-10-10
  • 修回日期:  2003-01-10
  • 刊出日期:  2003-03-10

目录

    盆山耦合与沉积盆地成因

      基金项目:  国家重点基础研究发展规划 ( 973)项目 G19990 4330 3课题资助
    • 中图分类号: P512.2

    摘要: 我国的沉积盆地成因研究主要遵循盆山耦合的研究思路进行 ,关注重点为盆山体系的构造、沉积和深部结构上的耦合现象。构造耦合研究是指盆山结合带的统一变形特征 ,沉积耦合研究是通过沉积响应去重塑盆山耦合过程及相邻造山带的演化过程 ,深部结构耦合的重点是研究盆山体系在岩石圈尺度的动力学统一性。国际上相应领域的研究重点为岩石圈深部过程与近地表构造过程的耦合。国内外研究既有相同之处 ,又有差异之处。建议在未来的沉积盆地成因研究中更加开阔思路 ,采用天然实验室的工作模式 ,进行多学科综合研究。

    English Abstract

    王清晨, 李忠. 盆山耦合与沉积盆地成因[J]. 沉积学报, 2003, 21(1): 24-30.
    引用本文: 王清晨, 李忠. 盆山耦合与沉积盆地成因[J]. 沉积学报, 2003, 21(1): 24-30.
    WANG Qing-chen, LI Zhong. Basin-Orogen Coupling and Origin of Sedimentary Basins[J]. Acta Sedimentologica Sinica, 2003, 21(1): 24-30.
    Citation: WANG Qing-chen, LI Zhong. Basin-Orogen Coupling and Origin of Sedimentary Basins[J]. Acta Sedimentologica Sinica, 2003, 21(1): 24-30.
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