The Relevance of High-frequency Analysis Artifacts to Remote Triggering

Research Article| September 01, 2011 The Relevance of High-frequency Analysis Artifacts to Remote Triggering Zhigang Peng; Zhigang Peng School of Earth and Atmospheric Sciences The Georgia Institute of Technology 311 Ferst Drive Atlanta, Georgia 30332-0340 U.S.A. zpeng@gatech.edu (Z. P.) 1School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, U.S.A. Search for other works by this author on: GSW Google Scholar Leland Timothy Long; Leland Timothy Long School of Earth and Atmospheric Sciences The Georgia Institute of Technology 311 Ferst Drive Atlanta, Georgia 30332-0340 U.S.A. zpeng@gatech.edu (Z. P.) 1School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, U.S.A. Search for other works by this author on: GSW Google Scholar Peng Zhao Peng Zhao School of Earth and Atmospheric Sciences The Georgia Institute of Technology 311 Ferst Drive Atlanta, Georgia 30332-0340 U.S.A. zpeng@gatech.edu (Z. P.) 1School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, U.S.A. 2NORSAR, Kjeller, Norway Search for other works by this author on: GSW Google Scholar Seismological Research Letters (2011) 82 (5): 654–660. https://doi.org/10.1785/gssrl.82.5.654 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Zhigang Peng, Leland Timothy Long, Peng Zhao; The Relevance of High-frequency Analysis Artifacts to Remote Triggering. Seismological Research Letters 2011;; 82 (5): 654–660. doi: https://doi.org/10.1785/gssrl.82.5.654 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 The high-frequency content observed in teleseisms recorded by seismometers can be produced either by the nonlinear behavior of seismometers and digitizers (Delorey et al. 2008; Hellweg et al. 2008) or by the real Earth response. The latter include scattering from small-scale heterogeneities during seismic wave propagation (e.g., Chen and Long 2000) and high-frequency radiations from the earthquake source (e.g., Peng et al. 2006) or near-surface regions near the recording site (Fischer et al. 2008). Recent studies have shown that large-amplitude surface waves generated by earthquakes at regional and teleseismic... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.