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Table 1 The statistic difference value between gravity gradient after downward continuation and the 220th-order model of the EGM2008

From: Inversion of the density structure of the lithosphere in the North China Craton from GOCE satellite gravity gradient data

Parameters

\({\text{d}}{\varvec{T}}_{xx}\)

\({\text{d}}{\varvec{T}}_{xz}\)

\({\text{d}}{\varvec{T}}_{yy}\)

\({\text{d}}{\varvec{T}}_{zz}\)

Mean

− 0.013

− 0.09

− 0.030

0.035

Sigma

0.33

0.42

0.64

0.71

  1. dT represents the difference value of gravity gradient between preprocessed GOCE data and EGM2008