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• W1989512110 abstract "Research Article| August 01, 2013 A slump in the trench: Tracking the impact of the 2011 Tohoku-Oki earthquake M. Strasser; M. Strasser 1Geological Institute, ETH Zurich, Sonneggstrasse 5, 8092 Zurich, Switzerland Search for other works by this author on: GSW Google Scholar M. Kölling; M. Kölling 2MARUM—Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany Search for other works by this author on: GSW Google Scholar C. dos Santos Ferreira; C. dos Santos Ferreira 2MARUM—Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany Search for other works by this author on: GSW Google Scholar H.G. Fink; H.G. Fink 2MARUM—Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany Search for other works by this author on: GSW Google Scholar T. Fujiwara; T. Fujiwara 3Japan Agency of Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-Cho, Yokosuka-city, Kanagawa 237-0061, Japan Search for other works by this author on: GSW Google Scholar S. Henkel; S. Henkel 4Institute of Geology and Mineralogy, University of Cologne, Zülpicher Strasse 49a, 50674 Cologne, Germany Search for other works by this author on: GSW Google Scholar K. Ikehara; K. Ikehara 5Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukaba, Ibaraki 305-8568, Japan Search for other works by this author on: GSW Google Scholar T. Kanamatsu; T. Kanamatsu 3Japan Agency of Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-Cho, Yokosuka-city, Kanagawa 237-0061, Japan Search for other works by this author on: GSW Google Scholar K. Kawamura; K. Kawamura 6Departement of Geosphere Science, Yamaguchi University, Yamaguchi City, Yamaguchi 753-8512, Japan Search for other works by this author on: GSW Google Scholar S. Kodaira; S. Kodaira 3Japan Agency of Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-Cho, Yokosuka-city, Kanagawa 237-0061, Japan Search for other works by this author on: GSW Google Scholar M. Römer; M. Römer 2MARUM—Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany Search for other works by this author on: GSW Google Scholar G. Wefer; G. Wefer 2MARUM—Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany Search for other works by this author on: GSW Google Scholar R/V Sonne Cruise SO219A; R/V Sonne Cruise SO219A Search for other works by this author on: GSW Google Scholar JAMSTEC Cruise MR12-E01 scientists JAMSTEC Cruise MR12-E01 scientists Search for other works by this author on: GSW Google Scholar Author and Article Information M. Strasser 1Geological Institute, ETH Zurich, Sonneggstrasse 5, 8092 Zurich, Switzerland M. Kölling 2MARUM—Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany C. dos Santos Ferreira 2MARUM—Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany H.G. Fink 2MARUM—Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany T. Fujiwara 3Japan Agency of Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-Cho, Yokosuka-city, Kanagawa 237-0061, Japan S. Henkel 4Institute of Geology and Mineralogy, University of Cologne, Zülpicher Strasse 49a, 50674 Cologne, Germany K. Ikehara 5Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukaba, Ibaraki 305-8568, Japan T. Kanamatsu 3Japan Agency of Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-Cho, Yokosuka-city, Kanagawa 237-0061, Japan K. Kawamura 6Departement of Geosphere Science, Yamaguchi University, Yamaguchi City, Yamaguchi 753-8512, Japan S. Kodaira 3Japan Agency of Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-Cho, Yokosuka-city, Kanagawa 237-0061, Japan M. Römer 2MARUM—Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany G. Wefer 2MARUM—Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany R/V Sonne Cruise SO219A JAMSTEC Cruise MR12-E01 scientists Publisher: Geological Society of America Received: 11 Feb 2013 Revision Received: 09 Apr 2013 Accepted: 09 Apr 2013 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2013 Geological Society of America Geology (2013) 41 (8): 935–938. https://doi.org/10.1130/G34477.1 Article history Received: 11 Feb 2013 Revision Received: 09 Apr 2013 Accepted: 09 Apr 2013 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Tools Icon Tools Get Permissions Search Site Citation M. Strasser, M. Kölling, C. dos Santos Ferreira, H.G. Fink, T. Fujiwara, S. Henkel, K. Ikehara, T. Kanamatsu, K. Kawamura, S. Kodaira, M. Römer, G. Wefer, R/V Sonne Cruise SO219A, JAMSTEC Cruise MR12-E01 scientists; A slump in the trench: Tracking the impact of the 2011 Tohoku-Oki earthquake. Geology 2013;; 41 (8): 935–938. doi: https://doi.org/10.1130/G34477.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract We present differential bathymetry and sediment core data from the Japan Trench, sampled after the 2011 Tohoku-Oki (offshore Japan) earthquake to document that prominent bathymetric and structural changes along the trench axis relate to a large (∼27.7 km2) slump in the trench. Transient geochemical signals in the slump deposit and analysis of diffusive re-equilibration of disturbed SO42– profiles over time constrain the triggering of the slump to the 2011 earthquake. We propose a causal link between earthquake slip to the trench and rotational slumping above a subducting horst structure. We conclude that the earthquake-triggered slump is a leading agent for accretion of trench sediments into the forearc and hypothesize that forward growth of the prism and seaward advance of the deformation front by more than 2 km can occur, episodically, during a single-event, large mega-thrust earthquake. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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