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.
它们产出的地质特征表明，岩石圈相对地幔对流体，持续或幕式地向西滑移。
明：以上
、词性分类均由互联网资源自动生成，部分未经过人工审核，其表
亦不代表本软件的观点；若发现问题，欢迎向我们指正。
