Three important Holocene tephras off the Pacific coast of the Tohoku region, Northeast Japan: Implications for correlating onshore and offshore event deposits

Author:

Ikehara Ken,Usami Kazuko,Kanamatsu Toshiya,Danhara Tohru,Yamashita Tohru

Funder

Geophysical and Geological Studies of Earthquakes and Tsunamis for off-Tohoku District, Japan

Regional Study on Hazard Mitigation Along the Nankai Trough

Ministry of Education, Culture, Sports, Science and Technology (MEXT)

Geological Survey of Japan (GSJ), AIST

Research Institute of Geology and Geoinformation, GSJ, AIST

Kakenhi “Japan Trench Deep-Sea Research Project for Assessing Shallow Seismic Slips and Their History

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference46 articles.

1. Estimation of the height of the Sanriku Jogan 11 earthquake-tsunami (A.D. 869) in the Sendai Plain;Abe;J. Seismol. Soc. Jpn.,1990

2. Paleoseismicity of the Cascadia subduction zone: evidence from turbidites off the Oregon-Washington margin;Adams;Tectonics,1990

3. Tephrochronology;Alloway,2007

4. Late Quaternary tephrostratigraphy of marine core KH94-3, LM-8 off Sanriku, Japan;Aoki;Quat. Res. (Daiyonki-kenkyu),2000

5. Late Quaternary tephrostratigraphy of marine cores collected during “Mirai” MR98-03 and MR99-K04 cruises;Aoki;Tech. Rep. JAMSTEC,2000

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