Cited by 115earthquake and tectonic studiesGeological formations and processesEarthquake and Tsunami Effects

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Tsunami-generated turbidity current of the 2011 Tohoku-Oki earthquake.

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Arai, Kazuno, Naruse, Hajime, Miura, Ryo, Kawamura, Kiichiro, Hino, Ryota, Ito, Yoshihiro, Inazu, Daisuke, Yokokawa, Miwa, Izumi, Norihiro, Murayama, Masafumi, Kasaya, Takafumi·2013·Geology

DOI 10.1130/g34777.1

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Abstract

We show the first real-time record of the turbidity current associated with a great earthquake; in this case with the Mw 9.0, 2011 Tohoku-Oki event.Turbidity current deposits (turbidites) have been used to estimate earthquake recurrence intervals from geologic records.Until now, however, there has been no direct of evidence for the large-scale earthquake in subduction plate margins.After the 2011 Tohoku-Oki earthquake and tsunami, an anomalous event on the sea floor consistent with a turbidity current was recorded by ocean bottom pressure recorders and ocean bottom seismometers deployed off Sendai.Freshly-emplaced turbidites were collected from a wide area of seafloor off the Tohoku coastal region.We analyzed these measurements and sedimentary records to determine conditions of the modern tsunamigenic turbidity current.We anticipate our discovery to be a starting point for more detailed characterization of modern tsunamigenic turbidites toward their identification in geologic records.

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Authors: Arai, K., Naruse, H., Miura, R., Kawamura, K., Hino, R., Ito, Y., Inazu, D., Yokokawa, M., Izumi, N., Murayama, M., & Kasaya, T.
Affiliations: Chiba University (JP)
Kyoto University (JP)
Nippon Marine Enterprises, Ltd. (Japan) (JP)
Yamaguchi University (JP)
Tohoku University (JP)
National Research Institute for Earth Science and Disaster Resilience (JP)
Osaka Institute of Technology (JP)
Hokkaido University (JP)
Marine Core Research Institute, Kochi University (JP)
Japan Agency for Marine-Earth Science and Technology (JP)
ORCID: Naruse, Hajime
Kawamura, Kiichiro
Hino, Ryota
Ito, Yoshihiro
Inazu, Daisuke
Izumi, Norihiro
Murayama, Masafumi
Kasaya, Takafumi
Venue: Geology
Publisher: Geological Society of America
Published: 2013-11
Volume: 41
Issue: 11
Pages: 1195-1198
ISSN: 0091-7613 (ISSN-L)
1943-2682
DOI: 10.1130/g34777.1
OpenAlex: W2086413892
Cited by: 115
References: 26
Citations by year: 2026: 5 · 2025: 5 · 2024: 6 · 2023: 7 · 2022: 8 · 2021: 12 · 2020: 9 · 2019: 11 · 2018: 8 · 2017: 9 · 2016: 9 · 2015: 11 · 2014: 15
FWCI: 11.60
Type: journal article
Language: en
Open access: green
petit.lib.yamaguchi-u.ac.jp
Locations: Geology (publishedVersion)
Institutional Repositories DataBase (IRDB) (submittedVersion)
Funders: Japan Society for the Promotion of Science (21107003, 22403004)
Topics: Physical Sciences › Earth and Planetary Sciences › Geophysics › earthquake and tectonic studies
Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
Physical Sciences › Engineering › Civil and Structural Engineering › Earthquake and Tsunami Effects
Keywords: turbidity currents, 2011 Tohoku-Oki earthquake, tsunami, turbidites, subduction zone, earthquake recurrence, ocean bottom seismometers, seafloor sedimentation, Sendai region

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Tsunami-generated turbidity current of the 2011 Tohoku-Oki earthquake.

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