<?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>S0016-71692024000200783</article-id>
<article-id pub-id-type="doi">10.22201/igeof.2954436xe.2024.63.1.1717</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Prediction of Fourier Amplitude Spectrum of Ground Motion in Mexico City from Subduction Thrust Earthquakes]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Arroyo]]></surname>
<given-names><![CDATA[Danny]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ordaz]]></surname>
<given-names><![CDATA[Mario]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Singh]]></surname>
<given-names><![CDATA[Shri K.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma Metropolitana Departamento de Materiales ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Ingeniería ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2024</year>
</pub-date>
<volume>63</volume>
<numero>2</numero>
<fpage>783</fpage>
<lpage>801</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692024000200783&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692024000200783&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692024000200783&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Mexico City, one of the largest cities in the world, experiences frequent, devastating interplate earthquakes that originate on the subduction thrust along the Pacific coast of Mexico more than 250 km away. A notorious example is the 19 September 1985 Michoacán earthquake (Mw 8.0) which killed ~ 10,000 persons and caused wide-spread destruction in the city. The main cause of seismic damage in Mexico City is its subsoil that amplifies the ground motion. In view of the seismic hazard faced by the city, a reliable estimation of ground motion during future earthquakes is of vital importance. We present a new ground motion prediction equation (GMPE) for the Fourier amplitude acceleration spectrum (FAS) from subduction thrust earthquakes along the Pacific coast of Mexico at the reference station, CU, located in the firm zone of Mexico City. The GMPE is derived via Bayesian regression analysis and is based on an enlarged set of recordings (1965-2020; 40 earthquakes; 250 &#8804; R&#8804; 500 km; 5 &#8804; Mw &#8804; 8.0). An important feature of the new GMPE is that it includes a term to model different attenuation along different ray paths. The inclusion of this term leads to a reduction in the aleatory variability of the GMPE, particularly at high frequencies. Since spectral amplification of seismic waves with respect to CU is known at many sites in the city, the FAS at these sites can be computed if it is known at CU. The new GMPE has been incorporated in a fully Fourier-based probabilistic seismic hazard analysis of Mexico City.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La CDMX, una de las ciudades más grandes del mundo, ha sufrido continuamente sismos destructivos que se originan en la interfaz de la zona de subducción en la costa del Pacífico a más de 250 km de distancia. Un ejemplo notable es el gran sismo de Michoacán del 19 de septiembre de 1985 el cual devasto la ciudad y provocó más de 10,000 víctimas. La causa principal de los daños es la gran amplificación del movimiento del suelo que se presenta en la CDMX. En vista del nivel de peligro sísmico a que está expuesta la ciudad es necesario contar con estimaciones precisas del movimiento del suelo durante eventos sísmicos futuros. Se presenta un modelo de atenuación (GMPE) del espectro de amplitudes de Fourier de la aceleración (FAS) del movimiento del suelo, en la estación de Ciudad Universitaria (CU) en la CDMX, durante sismos en la interfaz de subducción a lo largo de la Costa del Pacífico Mexicano con mecanismo de falla inverso. Se consideran registros entre 1965 a 2020 durante 40 sismos con magnitudes entre 5 y 8 a distancias entre 250 km y 500 km, lo cual representa un incremento considerable de registros respecto a los estudios previos. Como método de regresión se utilizó un esquema de regresión Bayesiano. Una característica importante del modelo propuesto es que incluye términos para modelar la atenuación a lo largo de diferentes trayectorias, se observó que la inclusión de estos términos conduce a una reducción en la variabilidad aleatoria del GMPE, particularmente en altas frecuencias. Dado que la amplificación de las ondas sísmicas con respecto a la estación CU se conoce en muchos sitios instrumentados en la CDMX es posible estimar el FAS en estos sitios si se conoce el FAS en la estación CU. El modelo propuesto ha sido incorporado en un análisis de peligro sísmico basado en el uso de FAS y ha dado lugar a los espectros de diseño sísmico de la nueva versión del Reglamento de Construcciones de la CDMX.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[GMPE]]></kwd>
<kwd lng="en"><![CDATA[FAS]]></kwd>
<kwd lng="en"><![CDATA[subduction earthquakes]]></kwd>
<kwd lng="en"><![CDATA[Bayesian analysis]]></kwd>
<kwd lng="es"><![CDATA[Modelo de atenuación]]></kwd>
<kwd lng="es"><![CDATA[espectro de amplitud de Fourier]]></kwd>
<kwd lng="es"><![CDATA[sismos de subducción]]></kwd>
<kwd lng="es"><![CDATA[análisis de regresión Bayesiano]]></kwd>
</kwd-group>
</article-meta>
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