<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "https://jats.nlm.nih.gov/nlm-dtd/publishing/3.0/journalpublishing3.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" specific-use="SMUR" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">SED</journal-id>
<journal-title-group>
<journal-title>Solid Earth Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">SED</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Solid Earth Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1869-9537</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/se-2019-191</article-id>
<title-group>
<article-title>An MCMC Bayesian full moment tensor inversion constrained by first-motion polarities and double couple percent</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pakzad</surname>
<given-names>Mehrdad</given-names>
<ext-link>https://orcid.org/0000-0002-7272-0205</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Khalili</surname>
<given-names>Mahnaz</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vahidravesh</surname>
<given-names>Shaghayegh</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Geophysics, University of Tehran, Tehran, 1435944411, Iran</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Graduate Student of Geophysics, Institute of Geophysics, University of Tehran, Tehran, 1435944411, Iran</addr-line>
</aff>
<pub-date pub-type="epub">
<day>27</day>
<month>01</month>
<year>2020</year>
</pub-date>
<volume>2020</volume>
<fpage>1</fpage>
<lpage>27</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2020 Mehrdad Pakzad et al.</copyright-statement>
<copyright-year>2020</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://se.copernicus.org/preprints/se-2019-191/">This article is available from https://se.copernicus.org/preprints/se-2019-191/</self-uri>
<self-uri xlink:href="https://se.copernicus.org/preprints/se-2019-191/se-2019-191.pdf">The full text article is available as a PDF file from https://se.copernicus.org/preprints/se-2019-191/se-2019-191.pdf</self-uri>
<abstract>
<p>&lt;p&gt;Monte Carlo Markov chain (MCMC) samplings can obtain a set of samples by directed random walk, mapping the posterior probability density of the model parameters in Bayesian framework. We perform earthquake waveform inversion to retrieve focal angles or the elements of moment tensor and source location using a Bayesian MCMC method with the constraints of first-motion polarities and double couple percentage using full Green functions and data covariance matrix. The algorithm tests the compatibility with polarities and also checks the double couple percentage of every site before the time-consuming synthetic seismogram computation for every sample of moment tensor of every trial source position. Other than large earthquakes, the method is especially suitable for weak events (M&amp;thinsp;&lt;&amp;thinsp;4) that their focal mechanisms cannot be well-constrained by polarities or seismograms alone, unless a dense local network is available; something that is generally occasional. Two- and one-station solutions show more agreement with all-station solution if polarity and DC&amp;thinsp;% constraints are employed. In order to examine the validity of the method, two events with the independent focal mechanism solutions are utilized. Furthermore, we also calculate data covariance matrix from pre-event noise and Green function uncertainty to obtain the errors of focal mechanisms.&lt;/p&gt;</p>
</abstract>
<counts><page-count count="27"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>