<?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>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742023000200174</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2023.2.1744</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Mapping the mineralogy in the Oxia Planum and Mawrth Vallis ExoMars landing sites - Implications for aqueous alteration and paleoenvironmental evolution]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Reyes Ayala]]></surname>
<given-names><![CDATA[Karen Itzel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Kajdi&#269;]]></surname>
<given-names><![CDATA[Primo&#382;]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Urrutia Fucugauchi]]></surname>
<given-names><![CDATA[Jaime]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Martínez-Frías]]></surname>
<given-names><![CDATA[Jesús]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vago]]></surname>
<given-names><![CDATA[Jorge L.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Durand Manterola]]></surname>
<given-names><![CDATA[Héctor]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González Torres]]></surname>
<given-names><![CDATA[Enrique Alejandro]]></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 ]]></institution>
<addr-line><![CDATA[Coyoacán Mexico City]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Complutense de Madrid Instituto de Geociencias ]]></institution>
<addr-line><![CDATA[Madrid ]]></addr-line>
<country>España</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Instituto de Investigación y Estudios Avanzados Chicxulub  ]]></institution>
<addr-line><![CDATA[Yucatán ]]></addr-line>
<country>México</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,European Space Agency European Space Research and Technology Centre ]]></institution>
<addr-line><![CDATA[Noordwijk ]]></addr-line>
<country>Países Bajos</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Universidad Nacional Autónoma de México Facultad de Ingeniería ]]></institution>
<addr-line><![CDATA[Coyoacán Mexico City]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<volume>40</volume>
<numero>2</numero>
<fpage>174</fpage>
<lpage>186</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742023000200174&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742023000200174&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742023000200174&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Mineralogical studies constitute one of the main tools to investigate geological processes on Mars. Here, the mineralogy of the ExoMars landing sites Oxia Planum and Mawrth Vallis is analysed based on multispectral datasets of the CRISM Compact Reconnaissance Imaging Spectrometer for Mars of Mars Reconnaissance Orbiter, TES Thermal Emission Spectrometer of Mars Global Surveyor and OMEGA Visible and Infrared Mineralogical Mapping Spectrometer of Mars Express are integrated and interpreted. Primary and secondary minerals of carbonates, oxides, silicates and sulphates mineral groups are characterized, with most minerals produced by aqueous alteration, with 35 mineral species identified, amongst which phyllosilicates are the dominant group. Coexisting mineral types point to distinct hydrothermal and alteration stages. Our investigation supports that water must have been present on early Mars on superficial and endogenous processes, causing direct precipitation and transformations of secondary minerals, with some not usually formed simultaneously. Hence, it is likely that species may have arisen at different times, due to changes of Martian climate. Some minerals may have formed in the subsurface. The Martian palaeoenvironments might include subaerial, underwater, and shallow subsurface hydrothermal systems, cold springs, alkaline lakes, sabkhas, and playas. Our results contribute to our understanding of the planned landing sites to prepare for what the ExoMars rover mission may encounter, highlighting the impact that water may have had on the mineral genesis, alteration processes and their astrobiological potential.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Los estudios mineralógicos constituyen una de las principales herramientas para investigar los procesos geológicos en Marte. En este trabajo se integra e interpreta la mineralogía de los sitios de aterrizaje de la misión ExoMars, Oxia Planum y Mawrth Vallis. Los datos fueron analizados con base en conjuntos de datos multiespectrales del Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) del Mars Reconnaissance Orbiter; del Espectrómetro de Emisión Térmica (TES) del Mars Global Surveyor y del espectrómetro de mapeo mineralógico visible e infrarrojo (OMEGA) del Mars Express. Se identificaron 35 especies minerales, entre las cuales los filosilicatos son el grupo dominante. Se caracterizaron los minerales primarios y secundarios pertenecientes a los grupos de carbonatos, óxidos, silicatos y sulfatos, la mayoría productos de alteración acuosa. La coexistencia de los minerales apunta a estadios hidrotermales producto de diferentes alteraciones, a diferentes procesos mineralogenéticos y a un pH heterogéneo de la solución de la cual precipitaron que dependía del ambiente local. Nuestra investigación apoya que el agua debió estar presente en Marte primitivo en procesos superficiales y endógenos, provocando precipitaciones directas y transformaciones a minerales secundarios, algunos de los cuales no suelen formarse simultáneamente. Es probable que las diferentes especies minerales hayan surgido en diferentes momentos, debido a los cambios en el clima marciano, incluso ciertos minerales pudieron haberse formado en el subsuelo. Algunos de los paleoambientes marcianos pueden incluir sistemas hidrotermales subaéreos, submarinos y superficiales, manantiales fríos, lagos alcalinos, sabkhas y playas. Nuestros resultados contribuyen a la comprensión de los sitios de aterrizaje planificados y ayudan a prepararse para lo que pueda encontrar el rover de la misión ExoMars, destacando el impacto que el agua pudo haber tenido en la génesis mineral, los procesos de alteración y su potencial astrobiológico.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Mars]]></kwd>
<kwd lng="en"><![CDATA[Mineralogy]]></kwd>
<kwd lng="en"><![CDATA[Aqueous alteration]]></kwd>
<kwd lng="en"><![CDATA[Paleoenvironments]]></kwd>
<kwd lng="en"><![CDATA[Oxia Planum]]></kwd>
<kwd lng="en"><![CDATA[Mawrth Vallis]]></kwd>
<kwd lng="en"><![CDATA[ExoMars Mission]]></kwd>
<kwd lng="es"><![CDATA[Marte]]></kwd>
<kwd lng="es"><![CDATA[Mineralogía]]></kwd>
<kwd lng="es"><![CDATA[Alteración acuosa]]></kwd>
<kwd lng="es"><![CDATA[Paleoambientes]]></kwd>
<kwd lng="es"><![CDATA[Oxia Planum]]></kwd>
<kwd lng="es"><![CDATA[Mawrth Vallis]]></kwd>
<kwd lng="es"><![CDATA[Misión ExoMars]]></kwd>
</kwd-group>
</article-meta>
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<volume>108</volume>
<page-range>1-16</page-range></nlm-citation>
</ref>
</ref-list>
</back>
</article>
