Unusually large earthquakes inferred from tsunami deposits along the Kuril trench View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2003-08

AUTHORS

Futoshi Nanayama, Kenji Satake, Ryuta Furukawa, Koichi Shimokawa, Brian F. Atwater, Kiyoyuki Shigeno, Shigeru Yamaki

ABSTRACT

The Pacific plate converges with northeastern Eurasia at a rate of 8-9 m per century along the Kamchatka, Kuril and Japan trenches. Along the southern Kuril trench, which faces the Japanese island of Hokkaido, this fast subduction has recurrently generated earthquakes with magnitudes of up to approximately 8 over the past two centuries. These historical events, on rupture segments 100-200 km long, have been considered characteristic of Hokkaido's plate-boundary earthquakes. But here we use deposits of prehistoric tsunamis to infer the infrequent occurrence of larger earthquakes generated from longer ruptures. Many of these tsunami deposits form sheets of sand that extend kilometres inland from the deposits of historical tsunamis. Stratigraphic series of extensive sand sheets, intercalated with dated volcanic-ash layers, show that such unusually large tsunamis occurred about every 500 years on average over the past 2,000-7,000 years, most recently approximately 350 years ago. Numerical simulations of these tsunamis are best explained by earthquakes that individually rupture multiple segments along the southern Kuril trench. We infer that such multi-segment earthquakes persistently recur among a larger number of single-segment events. More... »

PAGES

660

Journal

TITLE

Nature

ISSUE

6949

VOLUME

424

Author Affiliations

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/nature01864

DOI

http://dx.doi.org/10.1038/nature01864

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1001956476

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/12904789


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