<?xml version="1.0" encoding="UTF-8"?>
<article article-type="research-article" xml:lang="es" xmlns:xlink="http://www.w3.org/1999/xlink">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">global-journal-of-human-social-science-b-geography-environmental-science-disaster-management</journal-id>
<journal-title-group>
<journal-title>Global Journal of Human-Social Science - B: Geography, Environmental Science &amp; Disaster Management</journal-title>
</journal-title-group>
<issn publication-format="print">0975-587X</issn>
<issn publication-format="electronic">2249-460X</issn>
<publisher><publisher-name>Global Journals Publishing Group Incorporated</publisher-name></publisher>
<self-uri xlink:href="https://globaljournals.org/journal-seo-export/jats/61802.xml" />
</journal-meta>
<article-meta>
<article-id pub-id-type="publisher-id">61802</article-id>
<title-group>
<article-title>Seismotectonics Characterization of Mexico</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author"><name><surname>RodrÃ­guez</surname><given-names>Mario Octavio Cotilla</given-names></name><xref ref-type="aff" rid="aff1" />
</contrib>
<contrib contrib-type="author"><name><surname>Barba</surname><given-names>Diego CÃ³rdoba</given-names></name></contrib>
<contrib contrib-type="author"><name><surname>CornÃº</surname><given-names>Francisco Javier NÃºnez</given-names></name></contrib>
</contrib-group>
<aff id="aff1">MEXICO</aff>
<pub-date publication-format="electronic" date-type="pub" iso-8601-date="2021-07-15">
<day>15</day>
<month>07</month>
<year>2021</year>
</pub-date>
<volume>21</volume>
<issue>B4</issue>
<fpage>9</fpage>
<lpage>56</lpage>
<abstract><p>Mexico is an active Seismotectonic Region in the most part of North American continental plate and has 2 types of seismicity (interplate and intraplate). There are in the hierarchical structure 3 Seismotectonic Provinces (North Western, Western and Eastern Centre). Inside they exist 11 Seismotectonic Units where the Seismogenic Zones are defined. The last mentioned are segmented. Western Province has the highest level and where the contact of the converging plates take place.</p></abstract>
<kwd-group kwd-group-type="author-generated">
<kwd>active zones</kwd>
<kwd>mexico</kwd>
<kwd>seismic hazard</kwd>
<kwd>seismotectonic.</kwd>
</kwd-group>
<self-uri content-type="pdf" xlink:href="https://globaljournals.org/GJHSS_Volume21/2-Seismotectonics-Characterization.pdf" />
<self-uri content-type="html" xlink:href="https://globaljournals.org/scholarly-articles/seismotectonics-characterization-of-mexico/" />
</article-meta>
</front>
<body>
<sec>
<title>Full Text</title>
<p>Mexico is an active Seismotectonic Region in the most part of North American continental plate and has 2 types of seismicity (interplate and intraplate). There are in the hierarchical structure 3 Seismotectonic Provinces (North Western, Western and Eastern Centre). Inside they exist 11 Seismotectonic Units where the Seismogenic Zones are defined. The last mentioned are segmented. Western Province has the highest level and where the contact of the converging plates take place.</p>
</sec>
</body>
</article>