Geological charact eristics at their locations show continuous or pulsive westward slipping of lith osphere with respect to convection cell.
它们产出的地质特征
明，岩
圈相对地幔对流体，持续或幕式地向西
移。
“
”之义Geological charact eristics at their locations show continuous or pulsive westward slipping of lith osphere with respect to convection cell.
它们产出的地质特征明，岩圈相对地幔对流体，持续或幕式地向西移。
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