Geological charact eristics at their locations show continuous or pulsive westward slipping of lith osphere with respect to convection cell.
它们产出
特征表明，岩石圈相对幔对流体，持续或幕式向西滑移。
Geological charact eristics at their locations show continuous or pulsive westward slipping of lith osphere with respect to convection cell.
它们产出特征表明，岩石圈相对幔对流体，持续或幕式向西滑移。
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