Fig. 4From: Inversion of the density structure of the lithosphere in the North China Craton from GOCE satellite gravity gradient dataInterfacial relief-corrected anomalous gravity gradient component. a \({\varvec{T}}_{xx}\). b \({\varvec{T}}_{xz}\). c \({\varvec{T}}_{yy}\). d \({\varvec{T}}_{zz}\)Back to article page