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,岩石圈相对幔对流体,持续或幕式西。
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,岩石圈相对幔对流体,持续或幕式西。
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