The current inference of mantleflow is largely based on seismic tomography and anisotropic analysis.
地震波速度结构层析成像和地震各向异性分析,是推测现今地幔流动的主要观测依据。
2
It is consistent with the results obtained from other data. The possible mechanism is lithosphere plate motion and mantleflow.
这与用其它资料分析的结果一致,可能的机制是岩石圈板块运动和地幔对流。
3
With the new algorithms, the scientists were able tosimulate global mantleflow and how it manifests as plate tectonics and themotion of individual faults.