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Fig. 3 | Earth, Planets and Space

Fig. 3

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

Fig. 3

Bouguer anomaly distribution of the analyzed area. A low-pass filter with a cutoff wavelength of 10 km is applied. The assumed density of the terrain corrections is 2670 kg/m3. The continuous red lines show active faults (Nakata and Imaizumi 2002) and the broken red lines show the extended fault line of the Futagawa fault zone (HERP 2013a)

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