人们进行了一些地震学、地球化学方面的研究，这些研究中得出的数据和模型是一致的，但是它们不是最可靠的证据。
Some studies have been done, seismographic, geochemical, where the data's consistent with the model, but they aren't definitive proof.
记录地面运动的全波场，对地震学、地震勘探学以及地震模型试验都有重要的意义。
It is a great significant for surveying the full fields seismic movement in seismology and seismic prospecting as well as model seismology.
多方面的结果表明，地震学方法为当前流行的下地壳流动模型提供了深部证据。
From other researching aspects, the seismological method provides the evidences to support the flowing model of low mantle, which are popular in the researchers.
地震学、地球动力学研究倾向于全地幔对流模型；地球化学研究则支持分层地幔对流。
Seismological and geodynamical evidences supported whole mantle convection model, while geochemical ones supported layered convection model.
地震学、地球动力学研究倾向于全地幔对流模型；地球化学研究则支持分层地幔对流。
Seismological and geodynamical evidences supported whole mantle convection model, while geochemical ones supported layered convection model.
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