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• W2310888900 abstract "Research Article| November 01, 2015 Principal slip zones: Precursors but not recorders of earthquake slip Matt J. Ikari Matt J. Ikari * 1MARUM, Center for Marine Environmental Sciences, University of Bremen, D-28359 Bremen, Germany2Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA *E-mail: mikari@marum.de Search for other works by this author on: GSW Google Scholar Author and Article Information Matt J. Ikari * 1MARUM, Center for Marine Environmental Sciences, University of Bremen, D-28359 Bremen, Germany2Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA *E-mail: mikari@marum.de Publisher: Geological Society of America Received: 29 May 2015 Revision Received: 24 Aug 2015 Accepted: 26 Aug 2015 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2015 Geological Society of America Geology (2015) 43 (11): 955–958. https://doi.org/10.1130/G37028.1 Article history Received: 29 May 2015 Revision Received: 24 Aug 2015 Accepted: 26 Aug 2015 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Matt J. Ikari; Principal slip zones: Precursors but not recorders of earthquake slip. Geology 2015;; 43 (11): 955–958. doi: https://doi.org/10.1130/G37028.1 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 Narrow, highly-comminuted shear localization features in faults, known as principal slip zones (PSZs), are commonly associated with large-offset seismogenic faults. In this study, laboratory friction experiments were performed using shale and slate gouges where deformation was encouraged to localize at the gouge–wall-rock boundary. The slate gouges develop a black, narrow PSZ composed of densely packed submicron particles that appear sintered while the spectator gouge remains largely undeformed. These PSZs form at subseismic slip velocities of ∼10−5 m/s and with a calculated temperature rise of ∼3 °C. Instances of velocity-weakening friction, which is necessary for unstable fault slip, are only observed for slate samples with a PSZ; shale gouges, however, do not develop a PSZ and exhibit only velocity-strengthening frictional behavior. The development of a PSZ may therefore be a prerequisite for future earthquake slip to occur, rather than unequivocal evidence of past earthquake slip. 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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