<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Robert E. Kayen</dc:contributor>
  <dc:contributor>Brad Carkin</dc:contributor>
  <dc:contributor>Hajime Tanaka</dc:contributor>
  <dc:creator>Eric M. Thompson</dc:creator>
  <dc:date>2010</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;We present one-dimensional shear-wave velocity (&lt;/span&gt;&lt;i&gt;V&lt;sub&gt;S&lt;/sub&gt;&lt;/i&gt;&lt;span&gt;) profiles at 52 strong-motion sites that recorded the 28 September 2004 Magnitude 6.0 Parkfield, Calif., earthquake. We estimate the&amp;nbsp;&lt;/span&gt;&lt;i&gt;V&lt;sub&gt;S&lt;/sub&gt;&lt;/i&gt;&lt;span&gt;&amp;nbsp;profiles with the Spectral Analysis of Surface-Waves (SASW) method. The SASW method is a noninvasive method that indirectly estimates the&amp;nbsp;&lt;/span&gt;&lt;i&gt;V&lt;sub&gt;S&lt;/sub&gt;&lt;/i&gt;&lt;span&gt;&amp;nbsp;at depth from variations in the Rayleigh wave phase velocity at the surface. To address the uncertainty associated with these measurements, we compare the SASW profiles to surface-source downhole-receiver (SSDR) profiles at four sites. Three of the four SSDR sites are in close agreement with the adjacent SASW site, while the SASW profile is considerably slower than the SSDR profile at one site.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr20101168</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Surface-wave site characterization at 52 strong-motion recording stations affected by the Parkfield, California, M6.0 earthquake of 28 September 2004</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>