<?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>Thorne Lay</dc:contributor>
  <dc:contributor>Aaron A. Velasco</dc:contributor>
  <dc:contributor>John E. Vidale</dc:contributor>
  <dc:creator>Charles J. Ammon</dc:creator>
  <dc:date>1994</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;We describe two methods, suitable for routine application to teleseismic recordings, that characterize the time history of seismic events. Stacking short-period signals from large regional arrays provides stable estimates of high-frequency radiation from the source, and an empirical Green's function deconvolution procedure extracts reliable, broadband time functions suitable for analysis of faulting complexity and the spatio-temporal extent of rupture. Combined, these procedures characterize the source radiation of large events (&lt;/span&gt;&lt;i&gt;M&lt;sub&gt;s&lt;/sub&gt;&lt;/i&gt;&lt;span&gt; &amp;gt; 7) between 200- and 0.5-sec periods.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1785/BSSA0840041266</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Seismological Society of America</dc:publisher>
  <dc:title>Routine estimation of earthquake source complexity: The 18 October 1992 Colombian earthquake</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>