<?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>S0016-71692024000401341</article-id>
<article-id pub-id-type="doi">10.22201/igeof.2954436xe.2024.63.4.1752</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Reconstrucción geológica del área del ecoparque El Arenal, Sierra Chichinautzin, México: Implicaciones sobre el origen de los depósitos de ceniza en el cerro Magdalena]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Villalba]]></surname>
<given-names><![CDATA[Natalia Isabel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Guilbaud]]></surname>
<given-names><![CDATA[Marie-Noëlle]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,nataliai.villalbam@gmail.com  ]]></institution>
<addr-line><![CDATA[ Ciudad de México]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica Departamento de Vulcanología]]></institution>
<addr-line><![CDATA[Coyoacán 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>1341</fpage>
<lpage>1366</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692024000401341&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692024000401341&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692024000401341&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El parque ecoturístico El Arenal, ubicado en la parte norte del campo monogenético de la Sierra Chichinautzin, en el sur de la Ciudad de México, es conocido por presentar una duna, la cual está formada por ceniza volcánica depositada sobre el cerro Magdalena. Este trabajo se centra en caracterizar tanto el depósito de ceniza del ecoparque, como los productos volcánicos del área circundante, correspondientes a flujos y domos de lava y depósitos de caída, con el objetivo de determinar el origen y los procesos asociados con su depositación o emplazamiento, y así mismo, poder reconstruir la historia geológica del área del ecoparque. Los métodos usados constan de trabajos de campo, análisis de datos remotos (LIDAR y fotografías aéreas), fechamiento por radiocarbono, y diferentes análisis de laboratorio (granulometría, componentes, petrografía, y química total y mineral). En el área del ecoparque se identificaron seis unidades volcánicas que se encuentran estratigráficamente, de base a tope, de la siguiente manera: 1) Un domo dacítico conocido como cerro Magdalena, 2) un cono de escoria conocido como volcán Yololica, el cual tiene depósitos de caída y flujos de lava basálticos (22,000 cal AP), 3) depósitos de caída andesíticos, asociados a la erupción de la Pómez Tutti Frutti del volcán Popocatépetl, 4) depósitos de caída, principalmente andesíticos, del volcán Pelado, 5) la Ceniza Arenal, conformada por ceniza de tamaño medio, bien seleccionada, con estratificación cruzada, de composición andesítica y compuesta por fragmentos juveniles (sideromelana y taquilita) y accidentales (pómez y líticos), y 6) lavas basálticas del volcán Xitle. Con base en la caracterización de estas unidades, se propone que el depósito de ceniza del ecoparque se formó poco después de la erupción del volcán Pelado, debido a la removilización eólica de los depósitos de caída de este volcán, combinados con los depósitos subyacentes de la Pómez Tutti Frutti. El proceso de removilización ocurrió por tormentas de ceniza, que mezclaron y re-depositaron ambos depósitos de caída, formando una duna en el sotavento del cerro Magdalena; posteriormente, el material depositado en la zona más distal fue cubierto por las lavas del volcán Xitle.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Arenal ecotouristic park is located in the northern part of Sierra Chichinautzin Monogenetic Field, at the southern end of Mexico City. The park is renowned for its dune-shaped dark volcanic sand deposited on the older dome of Cerro Magdalena. This work aims to characterize the Arenal ash deposit as well as the products in the surrounding area, corresponding to fall deposits and lava flows and domes, to determine the origin and processes associated with their deposition or emplacement to reconstruct the geological history of the park area. The methods used consisted of field work, remote data analysis (LIDAR and aerial photos), radiocarbon dating, and different laboratory analyses (granulometry, clast componentry, petrography, whole-rock, and mineral chemistry). A sequence of six different volcanic units were identified which from bottom to top levels consists in: 1) A dacitic dome known as Cerro Magdalena, 2) a scoria cone known as Yololica volcano, which has basaltic fall deposits and lava flows (22.000 cal BP), 3) andesitic fall deposits related to the Tutti Frutti Pumice from Popocatépetl volcano, 4) mainly andesitic fall deposits from Pelado volcano, 5) The Arenal Ash made of medium-sized, well-sorted, andesitic ash that comprises juvenile (sideromelane and tachylite) and accidental fragments (pumice and lithics), and 6) basaltic lavas from Xitle volcano. Based on the characteristics of these units, we suggest that the Arenal ash deposit was formed soon after the Pelado volcano eruption, due to eolian remobilization of fall deposits from this volcano, combined with underlying Tutti Frutti pumice deposits. The remobilization process occurred by ash storms that mixed and re-deposited both fall deposits, producing a dune on Cerro Magdalena&#8217;s leeward slopes; later, the material deposited in the distal zone was covered by lava flows of the Xitle volcano.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Vulcanismo monogenético]]></kwd>
<kwd lng="es"><![CDATA[removilización y re-depositación de ceniza]]></kwd>
<kwd lng="es"><![CDATA[transporte eólico]]></kwd>
<kwd lng="es"><![CDATA[Campo Volcánico Sierra Chichinautzin]]></kwd>
<kwd lng="en"><![CDATA[Monogenetic vulcanism]]></kwd>
<kwd lng="en"><![CDATA[ash remobilization and re-deposit]]></kwd>
<kwd lng="en"><![CDATA[eolian transport]]></kwd>
<kwd lng="en"><![CDATA[Sierra Chichinautzin Volcanic Field]]></kwd>
</kwd-group>
</article-meta>
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