Fig. 7From: Inversion of the density structure of the lithosphere in the North China Craton from GOCE satellite gravity gradient dataThe remaining gravity gradient anomalies components. a \({\varvec{T}}_{xx}\). b \({\varvec{T}}_{xz}\). c \({\varvec{T}}_{yy}\). d \({\varvec{T}}_{zz}\), the cross sections at the latitude of 33.5°N, 37.5°N, and 41.5°N are displayedBack to article page