Fig. 4From: Gravity anomalies and lithospheric flexure around the Longmen Shan deduced from combinations of in situ observations and EGM2008 dataThe covariance values of the FGAs residuals between measurements and EGM2008 data change with the distance d between any two observation stations, and the linear fitting result of the covariance. a The covariance values of the residuals (\(C_{\text{res}}\)) change with the distance between two observation stations. b The linear fitting result of \(C_{\text{res}}\) and the covariance function \(\hat{C}_{\text{res}}\), which can be expressed as \(\hat{C}_{\text{res}} = C_{1} + C_{2} d\).\(C_{1}\) and \(C_{2}\) are the parameters of the covariance function, which are calculated by fitting the \(C_{\text{res}} > 0\) Back to article page