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    西藏措勤盆地构造特征与地壳缩短

    Tectonic division and crustal shortening in the Coqen Basin,Xizang

    • 摘要: 措勤盆地为青藏高原仅次于羌塘盆地的第二大海相盆地,笔者通过对盆地基底和盖层变形特征分析,将措勤盆地基底划分为北部拗陷、北部隆起、中部拗陷和南部隆起4个一级构造单元;盖层划分为北部拗褶带、北部冲断带、中部拗褶带、南部冲断带和南部拗褶带5个一级构造单元,并利用平衡剖面计算得到措勤盆地晚白垩世缩短约24%。

       

      Abstract: The Coqen Basin,Xizang is the second large-scale marine basin only smaller than the Qiangtang Basin on the Qinghai-Xizang Plateau.Tectonically,the basement of the Coqen Basin may be divided into four first-order tectonic units,i.e.,northern depression,northern uplift,central depression and southern uplift,while the cover may be separated into five first-order tectonic units,i.e.,northern downwarped zone,northern thrust fault zone,central downwarped zone,southern thrust fault zone and southern downwarped zone.The shortening rates during the Late Cretaceous are estimated at about 24% on the basis of the balanced cross-section calculations.

       

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