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Earth, Planets and Space
Fig. 6 | Earth, Planets and Space

Fig. 6

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

Fig. 6

Temperature at the certain depth and the four gravity gradient components caused by the temperature variations in the lithosphere. a The density variations at the 70 km in terms of the temperature variations. b The density variations at the 120 km in terms of the temperature variations. c \({\varvec{T}}_{xx}\). d \({\varvec{T}}_{xz}\). e \({\varvec{T}}_{yy}\). f \({\varvec{T}}_{zz}\)

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