We present a new analytical solution to compute the full-tensor gravity gradient due to a
body mass of uniform density with arbitrary geometry. The solution is an extension of an …

Many regions around the world require improved gravimetric data bases to support very
accurate geoid modeling for the modernization of height systems using GPS. We present a …

Crustal thickness (Moho surface relief) is closely related to geotectonic, which is the
predominant research topic in lunar geophysics. For lunar crustal depth inversion, to …

Statistical correlation function, including two-point function, is one of the popular methods to
digitize microstructure quantitatively. This paper investigated how to represent statistical …

Abstract ESA (European Space Agency) has released a series of new-generation Earth
gravity field models computed from gradiometry and GPS observations carried out aboard …

将有限功率地形法(或称Tesseroid 单元体球谐谱域正演法) 运用到月球地形的重力梯度计算中,
并通过圣杯任务(GRAIL) 得到的重力场模型系数和Moontopo720 地形模型数据 …

摘要重力空白区数据填补的一个主要方法是基于地壳均衡理论进行的, 该方法亦用于EGM
系列模型的构建中. 本文研究了地形数据在构制地形/均衡重力场模型中的应用 …

We present a new approach to estimate the density structure of shallow oceanic mantle by
inversion of localized geoid anomalies. Our method is based on Bayesian statistics and is …

Gravity gradiometers can identify subsurface mass anomalies. To use a gravity gradiometer
at a satellite altitude (50 kilometers) to detect subsurface water ice at the lunar poles, specific …

The Earth topographic masses are compensated by an isostatic adjustment. According to
the isostatic hypothesis a mountain is compensated by mass deficiency beneath it, where …