<?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>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222021000100014</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2021v73n1a280520</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Geoquímica y geocronología U-Pb de la cuarzodiorita de Sabanalarga y el gabro de Santa Fe, Colombia]]></article-title>
<article-title xml:lang="en"><![CDATA[Geochemistry and U-Pb geochronology of the Sabanalarga quartz-diorite and Santa Fe gabbro, Colombia]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Zapata-Villada]]></surname>
<given-names><![CDATA[Juan Pablo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Giraldo]]></surname>
<given-names><![CDATA[Wilmer]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez]]></surname>
<given-names><![CDATA[Gabriel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Geraldes]]></surname>
<given-names><![CDATA[Mauro Cesar]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Obando]]></surname>
<given-names><![CDATA[Milton]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Servicio Geológico Colombiano  ]]></institution>
<addr-line><![CDATA[Antioquia ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidade do Estado do Rio de Janeiro Faculdade de Geologia ]]></institution>
<addr-line><![CDATA[Rio de Janeiro ]]></addr-line>
<country>Brazil</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<volume>73</volume>
<numero>1</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222021000100014&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222021000100014&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222021000100014&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Durante el Cretáceo Superior, el margen noroccidental de Suramérica se caracterizó por presentar un ambiente tectónico complejo, representado por la acreción de múltiples terrenos y la generación de varios eventos magmáticos. La cuarzodiorita de Sabanalarga y el Gabro de Santa Fe, anteriormente descritos como una única unidad denominada "Batolito de Sabanalarga", presentaban múltiples diferencias entre sí y hoy son considerados dos plutones independientes, exponiendo dos de los eventos magmáticos del cretáceo superior. Ambos plutones emplazados en cortezas de diferente afinidad; el Gabro de Santa Fe emplazado en corteza tipo Plateau y arco de islas, mientras que la cuarzodiorita de Sabanalarga es emplazada en corteza continental del Complejo Cajamarca. Los análisis químicos de roca total realizados, presentaron anomalías de Nb-Ti, patrones de HFSE y REE en los diagramas multielementales característicos de rocas generadas en ambientes de subducción. El gabro de Santa Fe presenta características adakiticas no presentes en la cuarzodiorita de Sabanalarga. El bajo contenido Zr y relaciones (La/Yb)n vs Sr/Y &lt; 10 sugieren que el magma del Gabro de Santa Fe fue formado en ambiente oceánico, contrario a la cuarzodiorita de Sabanalarga con alto Zr y relaciones (La/Yb)n vs Sr/Y &gt; 10 que sugieren para este magma un origen en un ambiente continental. Se realizaron análisis U-Pb LA-ICP-Ms para ambos intrusivos: el Gabro de Santa Fe presentó edades entre 78.4 y 81.8 Ma y la cuarzodiorita de Sabanalarga edades entre 71.5 y 76.7 Ma. A la luz de los nuevos datos geoquímicos y geocronológicos se sugiere en este trabajo que el Gabro de Santa Fe y la cuarzodiorita de Sabanalarga son dos cuerpos diferentes sin relación temporal y cuya relación espacial es todavía debatible. Para el ambiente de formación de estos plutones se sugiere un modelo de doble subducción tipo Molucca.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT During the Upper Cretaceous the northwestern margin of South America was characterized by a complex tectonic environment represented by the accretion of multiple terranes and the generation of varied magmatic events. The Sabanalarga quartz-diorite and the Santa Fe Gabbro previously described as a single body called Sabanalarga Batholith, present multiple differences among themselves and today are considered two independent plutons, representing two of the upper Cretaceous magmatics events. Both plutons intrude crusts of different affinity; The Santa Fe Gabbro intrudes a Plateau-type and island arc crust while the Sabanalarga quartz-di-orite intrude into continental crust. The carried total rock chemical analysis showed anomalies of Nb-Ti, patterns of HFSE and REE in the multielemental diagrams indicatives of rocks generated in subduction environments. The Santa Fe Gabbro presents adakitic characteristics that are not pressent in the Sabanalarga quartz-diorite. The low Zr content and relations (La / Yb) n vs Sr / Y &lt; 10 .suggest that the Santa Fe Gabbro magma wassformed in an oceanic environment, contrary to the Sabanalarga quartz-diorite with high Zr and relationships (La / Yb) n vs Sr / Y&gt; 10 who suggest an origin in a continental environmentfor this magma. U-Pb LA ICPMs were analyzed for both intrusives: Santa Fe Gabbro showed ages between 78.4 and 81.8 Ma and Sabanalarga quartz-diorite ages between 71.5 and 76.7Ma. Due to the new geochemical and geochronological data, it is suggested that Santa Fe Gabbro and Sabanalarga quartz-diorite are two different bodies with no temporal relationship and whose spatial relationship is still debatable. Is suggested for the geological setting of formation for these plutons a double subduction model type Molucca.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[geoquímica]]></kwd>
<kwd lng="es"><![CDATA[U-Pb]]></kwd>
<kwd lng="es"><![CDATA[gabro de Santa Fe]]></kwd>
<kwd lng="es"><![CDATA[cuarzodiorita de Sabanalarga]]></kwd>
<kwd lng="en"><![CDATA[geochemistry]]></kwd>
<kwd lng="en"><![CDATA[U-Pb]]></kwd>
<kwd lng="en"><![CDATA[Santa Fe de gabbro]]></kwd>
<kwd lng="en"><![CDATA[Sabanalarga quartz-diorite]]></kwd>
</kwd-group>
</article-meta>
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