Relationship between the maximum extent of tsunami sand and the inundation limit of the 2011 Tohoku-oki tsunami on the Sendai Plain, Japan

Author:

Abe Tomoya,Goto Kazuhisa,Sugawara Daisuke

Funder

Tohoku University

Grant-in-Aid from JSPS

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference51 articles.

1. Estimation of the height of the Sanriku Jōgan 11 Earthquake-tsunami (A.D. 869) in the Sendai Plain;Abe;Journal of the Seismological Society of Japan (Zishin),1990

2. Tsunami inundation and sediment transport in a sediment-limited embayment on American Samoa;Apotsos;Earth-Science Reviews,2011

3. Chemical signatures of palaeotsunamis: a forgotten proxy?;Chagué-Goff;Marine Geology,2010

4. Chagué-Goff, C., Andrew, A., Szczuciński, W., Goff, J., Nishimura, Y., submitted for publication. Geochemical signatures up to the maximum inundation of the 2011 Tohoku-oki tsunami — implications for the 869 AD Jōgan and other palaeotsunamis. Sedimentary Geology.

5. Erosion and sedimentation from the 17 July, 1998 Papua New Guinea tsunami;Gelfenbaum;Pure and Applied Geophysics,2003

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