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