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Earth, Planets and Space
Fig. 2 | Earth, Planets and Space

Fig. 2

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

Fig. 2

a The gravity gradient effect \({\varvec{T}}_{zz}\) after average orbital correction to the altitude of 250 km. b The gravity gradient effect \({\varvec{T}}_{zz}\) after downward continuation to the altitude of 10 km. c The gravity gradient \({\varvec{T}}_{zz}\) with the 220th-order model of the EGM2008 at the altitude of 10 km. d The gravity gradient effect \({\varvec{T}}_{zz}\) caused by the topographic masses

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