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Fig. 6 | Earth, Planets and Space

Fig. 6

From: Continuity, segmentation and faulting type of active fault zones of the 2016 Kumamoto earthquake inferred from analyses of a gravity gradient tensor

Fig. 6

Normalized total horizontal derivative (TDX) distribution of the Bouguer anomaly shown in Fig. 3. A structural boundary is recognized as large degree isoline. The continuous black lines show active faults (Nakata and Imaizumi 2002) and the broken black lines show the extended fault line of the Futagawa fault zone (HERP 2013a)

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