Fig. 8From: Eigenvector of gravity gradient tensor for estimating fault dips considering fault typeBouguer anomalies on the profiles (after Toyama City 2013). The Bouguer density of 2260 kg/m3 is assumed. The “Kurehayama Fault” shown in this figure indicates a rough fault location by Toyama City (Toyama City 2013). The unit of the gravity anomaly is given in milligal, and mGal = 10−5 m/s2 Back to article page