The earthquakes following the pole shift will be no more wrenching than earthquakes due to plate adjustments under normal circumstances.
与正常情况下的板块调整造成的地震相比，极移后的地震不仅仅是猛烈。
A key aspect of plate tectonic theory is that on geologic time scales ocean basins are transient features, opening and closing as plates shift.
板块运动理论的一个关键点就是在地质历史的尺度内，海洋盆地的开合是因为板块转换，具有转换特征。
应用推荐