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