<?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>K.M. Larson</dc:contributor>
  <dc:contributor>Y. Tan</dc:contributor>
  <dc:contributor>K.W. Hudnut</dc:contributor>
  <dc:contributor>K. Choi</dc:contributor>
  <dc:creator>C. Ji</dc:creator>
  <dc:date>2004</dc:date>
  <dc:description>The slip history of the 2003 San Simeon earthquake is constrained by combining strong motion and teleseismic data, along with GPS static offsets and 1-Hz GPS observations. Comparisons of a 1-Hz GPS time series and a co-located strong motion data are in very good agreement, demonstrating a new application of GPS. The inversion results for this event indicate that the rupture initiated at a depth of 8.5 km and propagated southeastwards with a speed ???3.0 km/sec, with rake vectors forming a fan structure around the hypocenter. We obtained a peak slip of 2.8 m and total seismic moment of 6.2 ?? 1018 Nm. We interpret the slip distribution as indicating that the hanging wall rotates relative to the footwall around the hypocenter, in a sense that appears consistent with the shape of the mapped fault trace. Copyright 2004 by the American Geophysical Union.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/2004GL020448</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Slip history of the 2003 San Simeon earthquake constrained by combining 1-Hz GPS, strong motion, and teleseismic data</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>