计算重力布格异常

资 源 简 介

计算重力布格异常，并反演莫霍面起伏，主要采用Parker密度法反演

详 情 说 明

The text mentions the calculation of gravity Bouguer anomalies and the inversion of Moho surface relief using Parker density method. To elaborate, the Parker density method is a commonly used technique for the inversion of Bouguer anomalies to estimate the density distribution in the subsurface. It involves calculating the gravity field using Parker's method, which is based on the estimation of the density of the subsurface. The Moho surface, which is the boundary between the crust and mantle, can also be estimated using the inversion of Bouguer anomalies. The Moho depth is an important parameter that can be used to study the tectonic structure and evolution of a region. Therefore, the inversion of Bouguer anomalies using Parker density method is a crucial technique in geophysics and can provide valuable insights into the subsurface structure of the Earth.