<?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>Jon P. Stewart</dc:contributor>
  <dc:contributor>Emel Seyhan</dc:contributor>
  <dc:contributor>Gail M. Atkinson</dc:contributor>
  <dc:creator>David M. Boore</dc:creator>
  <dc:date>2013</dc:date>
  <dc:description>We provide ground-motion prediction equations for computing medians and standard deviations of average horizontal component intensity measures (IMs) for shallow crustal earthquakes in active tectonic regions. The equations were derived from a global database with M 3.0–7.9 events. We derived equations for the primary M- and distance-dependence of the IMs after fixing the V&lt;sub&gt;S30&lt;/sub&gt;-based nonlinear site term from a parallel NGA-West 2 study. We then evaluated additional effects using mixed effects residuals analysis, which revealed no trends with source depth over the M range of interest, indistinct Class 1 and 2 event IMs, and basin depth effects that increase and decrease long-period IMs for depths larger and smaller, respectively, than means from regional V&lt;sub&gt;S30&lt;/sub&gt;-depth relations. Our aleatory variability model captures decreasing between-event variability with M, as well as within-event variability that increases or decreases with M depending on period, increases with distance, and decreases for soft sites.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1193/070113EQS184M</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Earthquake Engineering Research Institute</dc:publisher>
  <dc:title>NGA-West 2 Equations for predicting PGA, PGV, and 5%-Damped PSA for shallow crustal earthquakes</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>