<?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>S0016-71692022000300201</article-id>
<article-id pub-id-type="doi">10.22201/igeof.00167169p.2022.61.3.2198</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[The Great 1822 Aleppo Earthquake: New Historical Sources and Strong Ground Motion Simulation]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Darawcheh]]></surname>
<given-names><![CDATA[Ryad]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Abdul-Wahed]]></surname>
<given-names><![CDATA[Mohamad Khir]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hasan]]></surname>
<given-names><![CDATA[Adnan]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Atomic Energy Commission of Syria Dept. of Geology ]]></institution>
<addr-line><![CDATA[Damascus ]]></addr-line>
<country>Syria</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>09</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>09</month>
<year>2022</year>
</pub-date>
<volume>61</volume>
<numero>3</numero>
<fpage>201</fpage>
<lpage>228</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692022000300201&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692022000300201&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692022000300201&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The devastating 1822 earthquake is one of the relatively recent events that struck northwestern Syria and the nearby areas of central-southern Turkey, at the junction of the Dead Sea fault system with the Eastern Anatolian fault system. This earthquake is re-examined, in this work, based on new original contemporary and near contemporary sources of information not cited in previous literature. Analysis of these sources reveals the following: (1) more detailed descriptions of the earthquake effects are provided for cities of Aleppo, Antakia and Latakia, and the identification of six new locations affected; (2) assessment of relevant earthquake parameters such as the epicenter, surface-wave, moment magnitudes and seismic intensity; (3) documentation of evidences of a seismic sea wave that occurred between the Cypriot and the Syrian coasts and (4) identification of the Saint Simeon fault, located to west of Aleppo, as the probable causative fault. Furthermore, the ground motion generated by the 1822 earthquake has been simulated using the extended stochastic simulation method. Acceleration time series and damped pseudo acceleration spectra were generated for Aleppo Citadel, where the peak ground acceleration, due to the earthquake, has been estimated at 0.4 g. The results will contribute to updating the seismic hazard setting in the northwestern Syria and central-southern Turkey.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El terremoto de 1822 fue devastador y se considera uno de los eventos relativamente recientes que azotaron el noroeste de Siria y las áreas cercanas del centro-sur de Turquía, es decir, en la unión del sistema de fallas del Mar Muerto con el sistema de fallas del este de Anatolia. En este trabajo, se vuelve a estudiar este terremoto, con base en nuevas fuentes de información originales contemporáneas y casi contemporáneas, que no habían sido citadas anteriormente. El análisis de estas fuentes revela lo siguiente: (1) se proporcionan descripciones más detalladas de los efectos del terremoto para las ciudades de Aleppo, Antakia y Latakia, y la identificación de seis nuevas ubicaciones afectadas; (2) evaluación de los parámetros pertinentes del terremoto, como el epicentro, la onda de superficie, las magnitudes de momento y la intensidad sísmica; (3) se muestra documentación de evidencias de una ola marina sísmica que ocurrió entre las costas chipriota y Siria, e (4) identificación de la falla de San Simeón, ubicada al oeste de Aleppo, como la probable falla causante. Además, el movimiento del suelo generado por el terremoto de 1822 ha sido simulado utilizando el método de estocástica extendida. Se generaron series temporales de aceleración y espectros de pseudoaceleración amortiguados para la ciudadela de Aleppo, donde la aceleración máxima del suelo, debido al terremoto, se estimó en 0.4 g. Los resultados contribuirán a actualizar la configuración de riesgo sísmico en el noroeste de Siria y el centro-sur de Turquía.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Terremotos históricos]]></kwd>
<kwd lng="es"><![CDATA[terremoto de Aleppo de 1822]]></kwd>
<kwd lng="es"><![CDATA[fuentes históricas de información]]></kwd>
<kwd lng="es"><![CDATA[simulación del movimiento del suelo]]></kwd>
<kwd lng="en"><![CDATA[Historical earthquakes]]></kwd>
<kwd lng="en"><![CDATA[The 1822 Aleppo earthquake]]></kwd>
<kwd lng="en"><![CDATA[Historical sources of information]]></kwd>
<kwd lng="en"><![CDATA[Ground motion simulation]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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