A Transportable System for Monitoring Ultralow Frequency Electromagnetic Signals Associated with Earthquakes (2000)

Research Article| July 01, 2000 A Transportable System for Monitoring Ultralow Frequency Electromagnetic Signals Associated with Earthquakes Darcy Karakelian; Darcy Karakelian Stanford University Department of Geophysics Stanford, CA 94305-2215 darcy@pangea.stanford.edu Search for other works by this author on: GSW Google Scholar Simon L. Klemperer; Simon L. Klemperer Stanford University Department of Geophysics Stanford, CA 94305-2215 darcy@pangea.stanford.edu Search for other works by this author on: GSW Google Scholar Antony C. Fraser-Smith; Antony C. Fraser-Smith Stanford University Department of Geophysics Stanford, CA 94305-2215 darcy@pangea.stanford.edu Search for other works by this author on: GSW Google Scholar Gregory C. Beroza Gregory C. Beroza Stanford University Department of Geophysics Stanford, CA 94305-2215 darcy@pangea.stanford.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Darcy Karakelian Stanford University Department of Geophysics Stanford, CA 94305-2215 darcy@pangea.stanford.edu Simon L. Klemperer Stanford University Department of Geophysics Stanford, CA 94305-2215 darcy@pangea.stanford.edu Antony C. Fraser-Smith Stanford University Department of Geophysics Stanford, CA 94305-2215 darcy@pangea.stanford.edu Gregory C. Beroza Stanford University Department of Geophysics Stanford, CA 94305-2215 darcy@pangea.stanford.edu Publisher: Seismological Society of America First Online: 09 Mar 2017 Online ISSN: 1938-2057 Print ISSN: 0895-0695 © 2000 by the Seismological Society of America Seismological Research Letters (2000) 71 (4): 423–436. https://doi.org/10.1785/gssrl.71.4.423 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Darcy Karakelian, Simon L. Klemperer, Antony C. Fraser-Smith, Gregory C. Beroza; A Transportable System for Monitoring Ultralow Frequency Electromagnetic Signals Associated with Earthquakes. Seismological Research Letters 2000;; 71 (4): 423–436. doi: https://doi.org/10.1785/gssrl.71.4.423 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 SocietySeismological Research Letters Search Advanced Search Claims that electromagnetic (EM) signals occur associated with some earthquakes, typically prior to but sometimes during seismic activity, have appeared in the literature for several decades (Parrot and Johnston, 1989; Park, et al., 1993; Park, 1996; Johnston, 1997). Such claims cover an exceptionally broad range of phenomena. For example, Gokhberg et al. (1982) and Yoshino (1991) observed increases in signal amplitude at 81 kHz from minutes to hours prior to earthquakes and up to hundreds of kilometers away from epicenters, and attributed these signals to seismoelectric emissions. Seismoelectric signals (SES) of... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.