Geological charact eristics at their locations show continuous or pulsive westward slipping of lith osphere with respect to convection cell.
它们产出的地
表明，岩石圈相对地幔对流体，持续或幕式地向西滑移。
Geological charact eristics at their locations show continuous or pulsive westward slipping of lith osphere with respect to convection cell.
它们产出的地表明，岩石圈相对地幔对流体，持续或幕式地向西滑移。
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