<?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>Bernard A. Chouet</dc:contributor>
  <dc:contributor>Phillip B. Dawson</dc:contributor>
  <dc:contributor>Peter M. Shearer</dc:contributor>
  <dc:contributor>Matthew M. Haney</dc:contributor>
  <dc:contributor>Gregory P. Waite</dc:contributor>
  <dc:contributor>Seth C. Moran</dc:contributor>
  <dc:contributor>T. Dylan Mikesell</dc:contributor>
  <dc:creator>Robin S. Matoza</dc:creator>
  <dc:date>2015</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Long-period (LP, 0.5-5&amp;thinsp;Hz) seismicity, observed at volcanoes worldwide, is a recognized signature of unrest and eruption. Cyclic LP &amp;ldquo;drumbeating&amp;rdquo; was the characteristic seismicity accompanying the sustained dome-building phase of the 2004&amp;ndash;2008 eruption of Mount St. Helens (MSH), WA. However, together with the LP drumbeating was a near-continuous, randomly occurring series of tiny LP seismic events (LP &amp;ldquo;subevents&amp;rdquo;), which may hold important additional information on the mechanism of seismogenesis at restless volcanoes. We employ template matching, phase-weighted stacking, and full-waveform inversion to image the source mechanism of one multiplet of these LP subevents at MSH in July 2005. The signal-to-noise ratios of the individual events are too low to produce reliable waveform-inversion results, but the events are repetitive and can be stacked. We apply network-based template matching to 8&amp;thinsp;days of continuous velocity waveform data from 29 June to 7 July 2005 using a master event to detect 822 network triggers. We stack waveforms for 359 high-quality triggers at each station and component, using a combination of linear and phase-weighted stacking to produce clean stacks for use in waveform inversion. The derived source mechanism pointsto the volumetric oscillation (~10&amp;thinsp;m&lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;) of a subhorizontal crack located at shallow depth (~30&amp;thinsp;m) in an area to the south of Crater Glacier in the southern portion of the breached MSH crater. A possible excitation mechanism is the sudden condensation of metastable steam from a shallow pressurized hydrothermal system as it encounters cool meteoric water in the outer parts of the edifice, perhaps supplied from snow melt.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1002/2015JB012279</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley</dc:publisher>
  <dc:title>Source mechanism of small long-period events at Mount St. Helens in July 2005 using template matching, phase-weighted stacking, and full-waveform inversion</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>