Paleoseismology and paleotsunamis of the NE Japan subduction ...

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Centennial geodetic data shows continuous (interseismic?) subsidence Nishimura (2012)
Kesen -numa To explain the Sanriku coastal data, either: 1) Gradual but episodic uplift occurs between earthquakes 2) 2011 M9 event typical, with long-term subsidence 3) A hidden huge event is still needed to uplift the coast
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 and 12: Onshore evidence for paleo-tsunamis
Page 13 and 14: Another way to infer seismic cycle
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 36: Major Outcomes • 350-550 years of

Paleoseismology and paleotsunamis of the NE Japan subduction ...

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