Geological charact eristics at their locations show continuous or pulsive westward slipping of lith osphere with respect to convection cell.
它们产出的
质特征表明，岩石圈
幔流体，持续或幕式向西
移。
Geological charact eristics at their locations show continuous or pulsive westward slipping of lith osphere with respect to convection cell.
它们产出的质特征表明，岩石圈幔流体，持续或幕式向西移。
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