Tsunami-generated turbidity current of the 2011 Tohoku-Oki earthquake.
Open accessAbstract
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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The AD 2011 Tohoku-oki earthquake remobilized young fine-grained surficial slope sediments enriched in organic matter, which was eventually deposited in the more than 7 km deep Japan Trench.
“In the hadal Japan Trench, the AD 2011 Tohoku-oki earthquake remobilized young fine-grained surficial slope sediments enriched in organic matter, which was eventually deposited in the more than 7 km deep trench (Arai et al., 2013; Oguri et al., 2013; Strasser et al., 2013; Ikehara et al., 2016; McHugh et al., 2016; Kanamatsu et al., 2017; Bao et al., 2018; Kioka et al., 2019; Molenaar et al., 2019”
From Event Stratigraphy in a Hadal Oceanic Trench: The Japan Trench as Sedimentary Archive Recording Recurrent Giant Subduction Zone Earthquakes and Their Role in Organic Carbon Export to the Deep Sea (2019) · cites this paper as Arai et al., 2013
The Introduction and Triggering Mechanism sections describe a turbidity current associated with the 2011 Tohoku-Oki tsunami, and the Characteristics section reports newly deposited, fine-grained sediment on the continental slope. Our copy does not establish that the remobilized sediment was young or enriched in organic matter, or that it was deposited in the Japan Trench at depths greater than 7 km; the reported instrument depths extend to 5700 m. (LLM, conf=0.88)
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Self-citation
- 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
- Venue
- Geology
- Publisher
- Geological Society of America
- Published
- 2013-11
- Volume
- 41
- Issue
- 11
- Pages
- 1195-1198
- ISSN
- 0091-7613 (ISSN-L)
- 1943-2682
- 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
- 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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