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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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Basin-Orogen Coupling and Origin of Sedimentary Basins

  • Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

  • Received Date: 2002-10-10
  • Rev Recd Date: 2003-01-10
  • Publish Date: 2003-03-10
  • The study on origin of sedimentary basins in China followed approach of basin-orogen (range) coupling, including the structural and sedimentary coupling, as well as coupling in deep structure. The structural coupling can be revealed with deformation in the place at which basin and orogen (range) are jointed. The sedimentary coupling implies the tectonic-sedimentary responses that could reconstruct the orogenic process. The coupling in deep structure focuses on lithosphere dynamics revealed by deep structures. Parallel to this, international study on origin of sedimentary basins concentrated on coupling of lithosphere and near-surface processes. Keeping open eyes, integrating different approaches, and co-working in natural laboratories are all important in the future research on sedimentary basins.
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  • Received:  2002-10-10
  • Revised:  2003-01-10
  • Published:  2003-03-10

Basin-Orogen Coupling and Origin of Sedimentary Basins

  • Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029
  • Received Date: 2002-10-10
  • Rev Recd Date: 2003-01-10
  • Publish Date: 2003-03-10

Abstract: The study on origin of sedimentary basins in China followed approach of basin-orogen (range) coupling, including the structural and sedimentary coupling, as well as coupling in deep structure. The structural coupling can be revealed with deformation in the place at which basin and orogen (range) are jointed. The sedimentary coupling implies the tectonic-sedimentary responses that could reconstruct the orogenic process. The coupling in deep structure focuses on lithosphere dynamics revealed by deep structures. Parallel to this, international study on origin of sedimentary basins concentrated on coupling of lithosphere and near-surface processes. Keeping open eyes, integrating different approaches, and co-working in natural laboratories are all important in the future research on sedimentary basins.

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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