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• W2096438699 abstract "Research Article| November 01, 2013 Mirror-like faults and power dissipation during earthquakes Michele Fondriest; Michele Fondriest * 1Dipartimento di Geoscienze, Università degli Studi di Padova, 35131 Padua, Italy2Istituto Nazionale di Geofisica e Vulcanologia (INGV), 00143 Rome, Italy *E-mail: michele.fondriest@studenti.unipd.it. Search for other works by this author on: GSW Google Scholar Steven A.F. Smith; Steven A.F. Smith 2Istituto Nazionale di Geofisica e Vulcanologia (INGV), 00143 Rome, Italy †Current address: Department of Geology, University of Otago, Dunedin 9054, New Zealand. Search for other works by this author on: GSW Google Scholar Thibault Candela; Thibault Candela 3Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA Search for other works by this author on: GSW Google Scholar Stefan B. Nielsen; Stefan B. Nielsen 2Istituto Nazionale di Geofisica e Vulcanologia (INGV), 00143 Rome, Italy Search for other works by this author on: GSW Google Scholar Karen Mair; Karen Mair 4Physics of Geological Processes, Department of Geosciences, University of Oslo, 0371 Oslo, Norway Search for other works by this author on: GSW Google Scholar Giulio Di Toro Giulio Di Toro 1Dipartimento di Geoscienze, Università degli Studi di Padova, 35131 Padua, Italy2Istituto Nazionale di Geofisica e Vulcanologia (INGV), 00143 Rome, Italy Search for other works by this author on: GSW Google Scholar Author and Article Information Michele Fondriest * 1Dipartimento di Geoscienze, Università degli Studi di Padova, 35131 Padua, Italy2Istituto Nazionale di Geofisica e Vulcanologia (INGV), 00143 Rome, Italy Steven A.F. Smith †Current address: Department of Geology, University of Otago, Dunedin 9054, New Zealand. 2Istituto Nazionale di Geofisica e Vulcanologia (INGV), 00143 Rome, Italy Thibault Candela 3Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA Stefan B. Nielsen 2Istituto Nazionale di Geofisica e Vulcanologia (INGV), 00143 Rome, Italy Karen Mair 4Physics of Geological Processes, Department of Geosciences, University of Oslo, 0371 Oslo, Norway Giulio Di Toro 1Dipartimento di Geoscienze, Università degli Studi di Padova, 35131 Padua, Italy2Istituto Nazionale di Geofisica e Vulcanologia (INGV), 00143 Rome, Italy *E-mail: michele.fondriest@studenti.unipd.it. Publisher: Geological Society of America Received: 11 Apr 2013 Revision Received: 21 Jul 2013 Accepted: 12 Aug 2013 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2013 Geological Society of America Geology (2013) 41 (11): 1175–1178. https://doi.org/10.1130/G34641.1 Article history Received: 11 Apr 2013 Revision Received: 21 Jul 2013 Accepted: 12 Aug 2013 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Michele Fondriest, Steven A.F. Smith, Thibault Candela, Stefan B. Nielsen, Karen Mair, Giulio Di Toro; Mirror-like faults and power dissipation during earthquakes. Geology 2013;; 41 (11): 1175–1178. doi: https://doi.org/10.1130/G34641.1 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 Earthquakes occur along faults in response to plate tectonic movements, but paradoxically, are not widely recognized in the geological record, severely limiting our knowledge of earthquake physics and hampering accurate assessments of seismic hazard. Light-reflective (so-called mirror like) fault surfaces are widely observed geological features, especially in carbonate-bearing rocks of the shallow crust. Here we report on the occurrence of mirror-like fault surfaces cutting dolostone gouges in the Italian Alps. Using friction experiments, we demonstrate that the mirror-like surfaces develop only at seismic slip rates (∼1 m/s) and for applied normal stresses and sliding displacements consistent with those estimated on the natural faults. Under these experimental conditions, the frictional power density dissipated in the samples is comparable to that estimated for natural earthquakes (1–10 MW/m2). Our results indicate that mirror-like surfaces in dolostone gouges are a signature of seismic faulting, and can be used to estimate power dissipation during ancient earthquake ruptures. 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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