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    HUANG Da-zhi, WANG Cheng-shan, DENG Lin. Developments in three-dimensional palaeogeographic and palaeotopographic reconstructions[J]. Sedimentary Geology and Tethyan Geology, 2001, 21(1): 88-92.
    Citation: HUANG Da-zhi, WANG Cheng-shan, DENG Lin. Developments in three-dimensional palaeogeographic and palaeotopographic reconstructions[J]. Sedimentary Geology and Tethyan Geology, 2001, 21(1): 88-92.

    Developments in three-dimensional palaeogeographic and palaeotopographic reconstructions

    • “Simulation technology” is an important tool for modern scientific research and has been applicable to geological research, e.g. basin simulation. According to mass-balanced palaeogeographic reconstructions proposed by Hay et al (1989), palaeogeography, palaeotopography and palaeobathymetry of a closed erosional depositional system can be reconstructed by restoring sedimentary masses to elevated surfaces in a drainage basin based on the inverse of present erosion equations and adjusting for isostasy, sea level changes, sediment compaction, and thermal subsidence. A mass balanced palaeogeographic reconstruction in integration with GIS techniques is a quantitative description of the configuration of the earth's surface at a moment in the geologic past based on sedimentary mass balance, and presents a three dimensional view of a sedimentary basin and its source area
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