<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692017000400377</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[A Simplified Method to Invert Slow Slip Events: Examples for the 2002, 2006 and 2014 events in Guerrero, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Castro Artola]]></surname>
<given-names><![CDATA[Oscar A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Iglesias]]></surname>
<given-names><![CDATA[Arturo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Kostoglodov]]></surname>
<given-names><![CDATA[Vladimir]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Franco-Sánchez]]></surname>
<given-names><![CDATA[Sara I.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hjörleifsdóttir]]></surname>
<given-names><![CDATA[Vala]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cabral-Cano]]></surname>
<given-names><![CDATA[Enrique]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Santoyo]]></surname>
<given-names><![CDATA[Miguel A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica Posgrado en Ciencias de la Tierra]]></institution>
<addr-line><![CDATA[México CDMX]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica ]]></institution>
<addr-line><![CDATA[México CDMX]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica Unidad Michoacán ]]></institution>
<addr-line><![CDATA[Morelia Michoacán]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2017</year>
</pub-date>
<volume>56</volume>
<numero>4</numero>
<fpage>377</fpage>
<lpage>389</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692017000400377&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692017000400377&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692017000400377&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract An efficient method to obtain a simple model of the slip distribution on a fault plane was developed from estimates of static offsets from continuous GPS measurements. Transfer functions were computed for the displacement due to a unit force on a fault plane (with a predetermined geometry, subdivided in a dense grid of subfaults) for all combinations of stations and subfaults, considering a layered media. The forward problem is built as a linear combination of elliptical slip-patches over the fault plane and the transfer functions between each patch and each station. To test the method, the 2002, 2006 and 2014 slow slip events (SSE) were modeled in Guerrero, Mexico, assuming that slip occurred along the subduction interface between the Cocos and North America plates. This subduction fault was modeled as two adjacent planes, both striking 289° for 600 km approximately parallel to the Middle America trench and with a width of 120 km (240 km total width). The shallower plane starts at the trench and dips 14° and the deeper plane is sub-horizontal (2° dip). The merged fault plane is segmented in 120x48, 5x5 km2 subfaults. A pre-calculated set of transfer functions is kept for future slow slip events, so that these only need to be computed for new GPS stations. A strong agreement between observations and synthetic data was found for all analyzed events, and the results are consistent with those reported by previous studies.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Se desarrolló un método eficiente para obtener un modelo simple de la distribución de deslizamientos en un plano de falla a partir de deformaciones estáticas observadas en mediciones continuas de GPS. Se calcularon funciones de transferencia; éstas representan el desplazamiento debido a una fuerza unitaria en un plano de falla (con una geometría predeterminada, subdividida en una malla densa de subfallas) para todas las combinaciones de estaciones y subfallas, considerando un medio estratificado. El problema directo se construye como una combinación lineal de parches elípticos de deslizamiento sobre el plano de falla y las funciones de transferencia. Para probar el método, se modelaron los eventos de deslizamiento lento (SSE, por sus siglas en inglés) de 2002, 2006 y 2014 en Guerrero, México, suponiendo que el movimiento ocurrió a lo largo de la interfase de subducción entre las placas de Cocos y Norteamérica. Se modeló la interfase de subducción como dos planos adyacentes, ambos con rumbo de 289° y por 600 km aproximadamente, y paralelos a la trinchera de América Central y con un ancho de 120 km (240 km de ancho total). El plano más somero comienza en la trinchera con un echado de 14°, mientras que el plano más profundo es sub-horizontal (2 ° dip). El plano de falla combinado está dividido en 120x48 subfallas de 5x5 km2. Un conjunto pre-calculado de funciones de transferencia se guarda para futuros eventos, de modo que éstas sólo necesitan ser calculadas para nuevas estaciones GPS. Se encontró un buen ajuste entre las observaciones y los datos cos para todos los eventos analizados, así como consistencia con resultados reportados en estudios previos.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Slow slip events]]></kwd>
<kwd lng="en"><![CDATA[slip inversion]]></kwd>
<kwd lng="en"><![CDATA[GPS application]]></kwd>
<kwd lng="en"><![CDATA[Middle America trench]]></kwd>
<kwd lng="en"><![CDATA[subduction]]></kwd>
<kwd lng="en"><![CDATA[Guerrero seismic gap]]></kwd>
<kwd lng="es"><![CDATA[Eventos de deslizamiento lento]]></kwd>
<kwd lng="es"><![CDATA[inversión de deslizamiento]]></kwd>
<kwd lng="es"><![CDATA[aplicación de GPS]]></kwd>
<kwd lng="es"><![CDATA[trinchera de Centro América]]></kwd>
<kwd lng="es"><![CDATA[subducción]]></kwd>
<kwd lng="es"><![CDATA[brecha sísmica de Guerrero]]></kwd>
</kwd-group>
</article-meta>
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