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.
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。
A method of gravity inversion for calculating basement of sedimentary basin using the data of seismic velocity spectrum, gravity anomalies, and water depth was built up.
建立了一种利用地震波速度谱、重力和水深资料反演沉积盆地基底的方法。
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