Response of natural smectite to seismogenic heating and potential implications for the 2011 Tohoku earthquake in the Japan Trench
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DOI:
10.1130/g36846.1
Publication Date:
2015-07-29T02:40:19Z
AUTHORS (3)
ABSTRACT
Research Article| September 01, 2015 Response of natural smectite to seismogenic heating and potential implications for the 2011 Tohoku earthquake in Japan Trench A.M. Schleicher; Schleicher 1Department Earth Environmental Sciences, University Michigan, 1100 N. Avenue, Ann Arbor, Michigan 48109, USA2Helmholtz Zentrum Potsdam, Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, 14473 Germany Search other works by this author on: GSW Google Scholar A. Boles; Boles USA B.A. van der Pluijm Geology (2015) 43 (9): 755–758. https://doi.org/10.1130/G36846.1 Article history received: 02 Apr rev-recd: 03 Jun accepted: 04 first online: 09 Mar 2017 Cite View This Citation Add Manager Share Icon Facebook Twitter LinkedIn MailTo Tools Get Permissions Site Schleicher, Boles, Pluijm; Trench. 2015;; doi: Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Dropdown Menu input auto suggest filter your All ContentBy SocietyGeology Advanced Abstract The sensitivity during brief protracted intervals can provide crucial information about temperature faults slip creep. Pelagic-sourced is most abundant clay mineral that incorporated into zone was drilled Fast Drilling Project (JFAST) Expedition 343 Trench, located ∼820 m below seafloor. study investigates preserve a record coseismic frictional associated with May laboratory examination hydration dehydration JFAST drill core samples (maximum 5 min) (5 h) sequences. Using real-time stage connected an X-ray diffractometer, we observe (1) both causes reduction water interlayers smectite, (2) recovers faster original state after quick than long heating, (3) nonrecoverable collapse all occurs at >200 °C rates. Because hydrated, clays are widely present fault rocks, conclude within cannot have reached significantly elevated temperatures. You do not access content, please speak institutional administrator if you feel should access.
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