摘要：In this paper, we propose an inverse method for full gravity gradient tensor data in the spherical coordinate system.As opposed to the traditional gravity inversion in the Cartesian coordinate system, our proposed method takes the curvature of the Earth, the Moon, or other planets into account, using tesseroid bodies to produce gravity gradient effects in forward modeling.We used both synthetic and observed datasets to test the stability and validity of the proposed method.Our results using synthetic gravity data show that our new method predicts the depth of the density anomalous body efficiently and accurately.Using observed gravity data for the Mare Smythii area on the moon, the density distribution of the crust in this area reveals its geological structure.These results validate the proposed method and potential application for large area data inversion of planetary geological structures.
关键词：Gravity gradient tensor; Inversion; Density distribution; Spherical coordinate system; Local north-oriented frame
