本文试图采用卫星重力资料和一种新的反演方法来研究地幔的横向密度异常分布。

In this paper, we attempt to use satellite gravity data and a new inversion method to study the lateral density anomalies distribution in the mantle.

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本文讨论利用重力资料反演莫霍面时，地壳横向不均一性，密度随深度变化以及异常数据滑动平均处理对解释结果的影响程度。

The lateral inhomogeneity and the variation of density contrast with depth in the crust and their effects on the inversion of gravity field are discussed.

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横向磁通电机由于可以获得较高的转矩密度现在正成为电机界研究的热点。

Because of the transverse flux machine can achieve high power density, it becomes a hotspot of electric machinery research.

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