<?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>Keith D. Koper</dc:contributor>
  <dc:contributor>William L. Yeck</dc:contributor>
  <dc:contributor>Sebastiano D’Amico</dc:contributor>
  <dc:contributor>Zongshan Li</dc:contributor>
  <dc:contributor>J. Mark Hale</dc:contributor>
  <dc:contributor>Relu Burlacu</dc:contributor>
  <dc:creator>Monique M. Holt</dc:creator>
  <dc:date>2019</dc:date>
  <dc:description>&lt;p&gt;In this paper we show that M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; is a viable and regionally portable depth discriminant and therefore may contribute in nuclear test ban treaty verification. A recent study found that the difference between local magnitude (M&lt;sub&gt;L&lt;/sub&gt;) and coda duration magnitude (M&lt;sub&gt;C&lt;/sub&gt;) discriminates shallow seismic events (mining blasts, mining-induced earthquakes, and shallow tectonic earthquakes) from deeper tectonic earthquakes in the Utah region. The shallow seismic events had anomalously high M&lt;sub&gt;C&lt;/sub&gt; values, with increasingly negative M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; values as depth decreased. Here we evaluate the performance of M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; as a depth discriminant in three new regions, finding that M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; increases between 0–9 km depth in all cases. Initially, we investigated M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; as a function of depth for naturally occurring earthquakes in the region around Yellowstone National Park, as recorded by the University of Utah Seismograph Stations. For 3,358 Yellowstone earthquakes with well-constrained depths, we found M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; increased 0.030 ± 0.007 magnitude units (m.u.) for each 1 km increase in depth up to 10 km depth. Next, we examined M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; values for anthropogenic seismicity in northern Oklahoma and southern Kansas, as recorded by the National Earthquake Information Center. For 1,628 events with well-constrained depths, we computed a slope for M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; of 0.022 ± 0.010 m.u./km. Finally, we analyzed M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; for 28,722 well-located earthquakes in Italy, as recorded by the National Institute of Geophysics and Volcanology, and found an M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; slope of 0.018 ± 0.001 m.u./km. In each case, the quoted error bounds represent 95% confidence regions which exclude zero, implying that the depth-dependence of M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; is statistically significant. We performed several robustness tests in which we varied the criterion used to define a well-constrained depth and the depth range used in the linear fit. In nearly all cases, we found a positive slope for M&lt;sub&gt;L&lt;/sub&gt;-M&lt;sub&gt;C&lt;/sub&gt; vs. depth at a confidence level above 95%.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1785/0120190096</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Seismological Society of America</dc:publisher>
  <dc:title>On the portability of ML-MC as a depth discriminant for small seismic events recorded at local distances</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>