Skip to main content
Fig. 4 | Earth, Planets and Space

Fig. 4

From: Gravity gradient tensor analysis to an active fault: a case study at the Togi-gawa Nangan fault, Noto Peninsula, central Japan

Fig. 4

Maps of the six components of gravity gradient tensor and indices (HD, VD, TDX, Di, \(\upbeta_{ \text{min} }\)) calculated from gravity gradient tensor components. White lines are active faults. Black lines in the VD (gzz) panel represent the zero isoline of VD. White and dark gray areas, respectively, in the Di panel indicate that whether the subsurface structure is approximately two-dimensional or three-dimensional. \(\upbeta_{ \text{min} }\) shows the dip angle of the subsurface structure

Back to article page