Attenuation Relationships for Shallow Crustal Earthquakes Based on California Strong Motion Data

Research Article| January 01, 1997 Attenuation Relationships for Shallow Crustal Earthquakes Based on California Strong Motion Data K. Sadigh; K. Sadigh Geomatrix Consultants 100 Pine St., l0th Floor San Francisco, CA 94111 Search for other works by this author on: GSW Google Scholar C.-Y. Chang; C.-Y. Chang Geomatrix Consultants 100 Pine St., l0th Floor San Francisco, CA 94111 Search for other works by this author on: GSW Google Scholar J.A. Egan; J.A. Egan Geomatrix Consultants 100 Pine St., l0th Floor San Francisco, CA 94111 Search for other works by this author on: GSW Google Scholar F. Makdisi; F. Makdisi Geomatrix Consultants 100 Pine St., l0th Floor San Francisco, CA 94111 Search for other works by this author on: GSW Google Scholar R.R. Youngs R.R. Youngs Geomatrix Consultants 100 Pine St., l0th Floor San Francisco, CA 94111 Search for other works by this author on: GSW Google Scholar Seismological Research Letters (1997) 68 (1): 180–189. https://doi.org/10.1785/gssrl.68.1.180 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation K. Sadigh, C.-Y. Chang, J.A. Egan, F. Makdisi, R.R. Youngs; Attenuation Relationships for Shallow Crustal Earthquakes Based on California Strong Motion Data. Seismological Research Letters 1997;; 68 (1): 180–189. doi: https://doi.org/10.1785/gssrl.68.1.180 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search nav search search input Search input auto suggest search filter All ContentBy SocietySeismological Research Letters Search Advanced Search Abstract Attenuation relationships are presented for peak acceleration and response spectral accelerations from shallow crustal earthquakes. The relationships are based on strong motion data primarily from California earthquakes. Relationships are presented for strike-slip and reverse-faulting earthquakes, rock and deep firm soil deposits, earthquakes of moment magnitude M 4 to 8+, and distances up to 100 km. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not currently have access to this article.