<?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>S0016-71692024000401241</article-id>
<article-id pub-id-type="doi">10.22201/igeof.2954436xe.2024.63.4.1769</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Reconstrucción del paleo-relieve del área del Volcán Xitle (Ciudad de México) y su impacto en la trayectoria de sus derrames de lava mediante simulaciones probabilísticas]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sandoval García]]></surname>
<given-names><![CDATA[Mariana]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Nieto-Torres]]></surname>
<given-names><![CDATA[Amiel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Martin Del Pozzo]]></surname>
<given-names><![CDATA[Ana Lillian]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,aff1  ]]></institution>
<addr-line><![CDATA[ Ciudad de México]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto Milenio de Investigación en Riesgo Volcánico-Ckelar Volcanes  ]]></institution>
<addr-line><![CDATA[Antofagasta ]]></addr-line>
<country>Chile</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,UNAM Instituto de Geofísica departamento de Vulcanología]]></institution>
<addr-line><![CDATA[ Ciudad de México]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2024</year>
</pub-date>
<volume>63</volume>
<numero>4</numero>
<fpage>1241</fpage>
<lpage>1263</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692024000401241&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692024000401241&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692024000401241&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La topografía prexistente jugó un papel fundamental en definir la trayectoria de los derrames de lava del Xitle. El Xitle es de los volcanes monogenéticos más jóvenes del sur de la Ciudad de México. Su erupción se caracterizó por emisiones menores de ceniza y de nueve derrames de lava pahoehoe y aa que cubrieron 78.94 km2. En este trabajo se reconstruyó el paleo-relieve del área del volcán Xitle para mejorar el conocimiento del paleo-drenaje y cómo determinó la trayectoria de los derrames de lava y la formación de tubos de lava. Se identificaron los depósitos de los volcanes pre-Xitle (Complejo Volcánico San Miguel, Ajusco, Cuilotepec, Coatzontle, Yololica y Malinale) según la morfología del relieve actual. Se modificaron las curvas de nivel del relieve actual para eliminar la topografía de los derrames de lava del Xitle y mediante la creación de una superficie ráster a partir de un TIN, se obtuvo un modelo digital de elevación del paleo-relieve. La distribución de los paleo-ríos se definió mediante el análisis de la acumulación y dirección de flujo en el paleo-relieve. Los derrames de lava del Xitle se simularon individualmente en el paleo-relieve con el programa probabilístico Q-LavHA. Se integraron las observaciones hechas en campo y estudios previos del volcán Xitle para definir los parámetros de las simulaciones de los derrames. Los derrames de lava del volcán Xitle cubrieron los depósitos de los volcanes pre-Xitle con excepción de las partes más altas como el caso del cono del volcán Cuilotepec y los montículos (hummocks) del Ajusco. Las lavas modificaron los cauces de algunos paleo-ríos (e.g. Magdalena) y rellenaron por completo otros (e.g. Cuicuilco). Las simulaciones muestran que las trayectorias de los derrames y la existencia y distribución de los tubos de lava están asociados a variaciones en la tasa de efusión, la disposición de los paleo-ríos, la morfología de los depósitos pre-Xitle y la abrupta pendiente del paleo-relieve.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Preexisting topography played a major role in defining the distribution of the Xitle lava flows. Xitle is one of the youngest monogenetic volcanoes in southern Mexico City. The eruption was characterized by small ash emissions and nine pahoehoe and aa lava flows that covered 78.94 km2. In this paper, the paleo-topography of the Xitle volcano area was reconstructed to improve knowledge of the paleo-drainage and how it determined the trajectory of the lava flows and the formation of lava tubes. Deposits of pre-Xitle volcanoes (San Miguel Volcanic Complex, Ajusco, Cuilotepec, Coatzontle, Yololica and Malinale) were identified according to the morphology of the current relief. The contour lines of the present-day relief were modified to eliminate the topography left by the Xitle lava flows. The modified contour lines were then processed creating a raster surface from a TIN to obtain the digital elevation model of the paleo-relief. The distribution of the paleo-channels was defined by analyzing the accumulation and direction of flow in the paleo-relief. Lava flows were individually simulated in the paleo-relief with the probabilistic program Q-LavHA. Field observations and previous studies were integrated to define the parameters of lava flow simulations. Lava flows from the Xitle volcano covered the deposits of the pre-Xitle volcanoes except for the highest parts, such as ones from the Cuilotepec cone and the Ajusco hummocks. The lava flows also partially filled and modified some paleo river-channels (e.g. Magdalena), and completely filled others (e.g. Cuicuilco). The simulations show that the trajectory of lava flows and the existence and distribution of lava tubes are associated with variations in the effusion rate, arrangement of the paleo river-channels, morphology of the pre-Xitle deposits and the abrupt slope.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Derrame de lava]]></kwd>
<kwd lng="es"><![CDATA[paleo-relieve]]></kwd>
<kwd lng="es"><![CDATA[paleo-ríos]]></kwd>
<kwd lng="es"><![CDATA[simulación]]></kwd>
<kwd lng="es"><![CDATA[reconstrucción]]></kwd>
<kwd lng="en"><![CDATA[Lava flows]]></kwd>
<kwd lng="en"><![CDATA[paleo-relief]]></kwd>
<kwd lng="en"><![CDATA[paleo-river]]></kwd>
<kwd lng="en"><![CDATA[simulation]]></kwd>
<kwd lng="en"><![CDATA[reconstruction]]></kwd>
</kwd-group>
</article-meta>
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