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Sakaguchi, Arito et al. (2011): Episodic seafloor mud brecciation due to great subduction zone earthquakes
Leg/Site/Hole:
Related Expeditions:
IODP 316
Identifier:
ID:
2011-097142
Type:
georefid
ID:
10.1130/G32043.1
Type:
doi
Creator:
Name:
Sakaguchi, Arito
Affiliation:
JAMSTEC (Japan Agency for Marine-Earth Science and Technology), IFREE (Institute for Frontier Research on Earth Evolution), Yokohama, Japan
Role:
author
Name:
Kimura, Gaku
Affiliation:
University of Tokyo, Japan
Role:
author
Name:
Strasser, Michael
Affiliation:
University of Bremen, Germany
Role:
author
Name:
Screaton, Elizabeth J.
Affiliation:
University of Florida, United States
Role:
author
Name:
Curewitz, Daniel
Affiliation:
Syracuse University, United States
Role:
author
Name:
Murayama, Masafumi
Affiliation:
Kochi University, Japan
Role:
author
Identification:
Title:
Episodic seafloor mud brecciation due to great subduction zone earthquakes
Year:
2011
Source:
Geology (Boulder)
Publisher:
Geological Society of America (GSA), Boulder, CO, United States
Volume:
39
Issue:
10
Pages:
919-922
Abstract:
The Nankai Trough off southwest Japan has an approximately 1300 yr historical record of great earthquakes, including the most recent, the A.D. 1944 Tonankai (M = 8.2) earthquake. Evaluation of the activity of an individual submarine fault is difficult when only onland observations are available. Submarine core records can pinpoint individual fault activity. Here we present Integrated Ocean Drilling Program (IODP) Nankai Trough Seismogenic Zone Experiment data from the shallow portion. IODP Expedition 316 drilled and cored several holes in the shallow portion of the offshore Tonankai earthquake area, including sites in the hanging wall of a margin-dominating splay fault that has previously been interpreted to have ruptured coseismically during megathrust earthquakes. X-ray computed tomography scanning revealed that the uppermost core at one site contains repeated occurrences of mud breccia. Radioisotope dating of the uppermost mud breccia indicates a deposition time consistent with the 1944 Tonankai earthquake, suggesting that the mud-breccia layers result from episodic brecciation caused by seismic shaking. Mud brecciation provides a potential new tool to reconstruct ancient earthquake history in subduction zones.
Language:
English
Genre:
Serial
Rights:
URL:
Coverage:
Geographic coordinates:
North:33.1400
West:136.4300
East: 136.4800
South:33.0100
Keywords:
Seismology; Asia; breccia; brecciation; clastic sediments; computed tomography data; cores; coseismic processes; deep-sea environment; earthquakes; Expedition 316; Far East; faults; great earthquakes; Integrated Ocean Drilling Program; Japan; marine environment; marine sediments; mud; Nankai Trough; NanTroSEIZE; North Pacific; Northwest Pacific; Pacific Ocean; paleoseismicity; periodicity; reconstruction; sediments; splay faults; subduction zones; Tonankai earthquake 1944; troughs; West Pacific;
.
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