结果表明，该区地壳深部速度结构与构造在纵向和横向上具有明显的不均一性。
The results show strong vertical and lateral inhomogeneity in deep crust velocity structure and tectonics.
由于空中大气介质的不均匀性使得电波传播速度减慢射线产生弯曲，从而产生折射误差。
The radio wave propagation velocity is slowed and the ray producing bend but to the asymmetry of the atmospheric medium, the refraction error is produced.
云南地区S波速度结构具有很强的横向不均匀性。
In Yunnan region, s wave velocity structures show strong horizontal heterogeneity.
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