ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
青藏高原莫霍面形态的重力模拟及其对探讨高原隆升机制的意义
  
关键词:Moho variation  gravity modelling  uplift  PKP residuals  Tibetan plateau
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作者单位
吕庆田 中国地质科学院矿床地质研究所 
姜枚 中国地质科学院矿床地质研究所 
高锐 中国地质科学院地质研究所 
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摘要:
The Gravity Modelling of Moho Variations and Its Significance to Uplift of Tibetan Plateau
      Tibetan Plateau is a large deformation zone produced by the collision between lndia and Euro-Asia, The deformation of lithosphere upper mantle play an crucial role in the uplift of Plateau. In this paper, the PKP residual variations along the central Tibetan profile is analysed and found that Moho steps are the common features beneath Tibetan Plateau. The gravity modelling is performed constrained by the seismic reflection data. It is suggested that folding, steps and imbrications of Moho may be the important mechamism related to the uplift of Tibetan Plateau. Finally, we discussed the influence of the plate motion, local thermal and density heterogeneity and mantle flow on the lithosphere deformaion.
LÜ Qing-tian,JIANG Mei,GAO Rui.1997.The Gravity Modelling of Moho Variations and Its Significance to Uplift of Tibetan Plateau[J].Acta Geoscientica Sinica,18(1):78-86.
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