The formation and evolution of the basin are considered to be constrained by the formation and waning of mantle plumes and stress processes of the Himalayan orogeny.

 
  • 柴達木第三紀轉換裂陷盆地形成演化主要受控于地幔熱柱的形成和衰減作用 ,同時(shí)喜馬拉雅運動(dòng)等運程應力作用對盆地的演化至關(guān)重要。
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