Paleoseismology and paleotsunamis of the NE Japan subduction ...

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Together with the Sendai and Fukushima data, large tsunamis might have occurred every 350-550 years Sawai et al. (2007)
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Page 1 and 2: Paleoseismology and paleotsunamis o
Page 3 and 4: To reveal the seismic cycle of M9 e
Page 5 and 6: Back marsh inundated by the 2011 ts
Page 7 and 8: 800-m-apart two cores share the sam
Page 9 and 10: Offshore tsunami deposits from Otsu
Page 11: Onshore evidence for paleo-tsunamis
Page 15 and 16: April 11, 2012 earthquake (Mw 6.6):
Page 17 and 18: Trenches across the Itozawa fault e
Page 19 and 20: Trench walls at Tsunagi, northern I
Page 21 and 22: A group of normal faults in Fukushi
Page 23: Older marine terraces (680-850 ka)
Page 34 and 35: Centennial geodetic data shows cont
Page 36: Major Outcomes • 350-550 years of

Paleoseismology and paleotsunamis of the NE Japan subduction ...

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