<?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 A. Page</dc:contributor>
  <dc:creator>David M. Boore</dc:creator>
  <dc:date>1972</dc:date>
  <dc:description>&lt;p&gt;Peak ground accelerations recently recorded within 10-15 km of faulting during moderate-sized earthquakes (m = 4 to 6) are significantly underestimated by many, if not most, of the empirical acceleration-distance relations commonly used in seismic engineering. The recent data show a rapid decrease of peak acceleration with increasing distances (at a rate between r&lt;sup&gt;-1.4&lt;/sup&gt; and&amp;nbsp; r&lt;sup&gt;-I.8&lt;/sup&gt;) beyond 5 to 20 km and suggest a less rapid rate of attenuation closer to the causative fault.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr7243</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Accelerations near faults that have moved during moderate-sized earthquakes</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>