Abstract
The Qinghai-Tibet Plateau is the largest plateau in the world, and the study of its Moho surface is of great significance to understand the deep structure and evolution of the earth. Aiming at the problem of insufficient vertical resolution of gravity data, the wavelet multi-scale analysis method is used to decompose the GOCE gravity gradient data along the Qinghai-Tibet Plateau, and the power spectrum analysis method is used to estimate the buried depth of the field source of the gravi
基于GOCE沿轨重力梯度反演青藏高原地壳结构-16722字.docx