摘要
We describe a method to perform a constrained lithospheric-scale inversion of satellite gravity gradient data.The a priori constraints include:i)data covariance matrix;ii)prior model covariance matrix including a model for spatial variability of mantle heterogeneity.
基金
supported by the European Space Agency’s Support to Science Element program,project"3D Earth:A Living Dynamics Planet"
performed at The Centre for Earth Evolution and Dynamics,University of Oslo,funded by the Research Council of Norway through its center of excellence funding scheme,project 223272
IPG SB RAS Project AAAAA16-116122810045-9
