<?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>0120-0283</journal-id>
<journal-title><![CDATA[Boletín de Geología]]></journal-title>
<abbrev-journal-title><![CDATA[bol.geol.]]></abbrev-journal-title>
<issn>0120-0283</issn>
<publisher>
<publisher-name><![CDATA[Universidad Industrial de Santander]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0120-02832019000200045</article-id>
<article-id pub-id-type="doi">10.18273/revbol.v41n2-2019003</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Aportes al conocimiento del Magmatismo de la Cordillera Central de Colombia en su Flanco Oriental: Área geotérmica de San Diego, Samaná, Caldas]]></article-title>
<article-title xml:lang="en"><![CDATA[Contributions to the Magmatism knowledge of the Central Cordillera of Colombia in its Eastern Flank: Geothermal Area of San Diego, Samaná, Caldas]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rueda-Gutiérrez]]></surname>
<given-names><![CDATA[Jesús Bernardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Servicio Geológico Colombiano Grupo de Exploración e Investigación en Recursos Geotérmicos ]]></institution>
<addr-line><![CDATA[Bogotá ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>08</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>08</month>
<year>2019</year>
</pub-date>
<volume>41</volume>
<numero>2</numero>
<fpage>45</fpage>
<lpage>70</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0120-02832019000200045&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0120-02832019000200045&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0120-02832019000200045&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Fueron caracterizados en el área geotérmica de San Diego, cinco cuerpos plutónicos, cuyas características químicas posicionan a cuatro unidades (Stock de Florencia, Batolito de Sonsón, Complejo de Samaná y Alaskita de Samaná) en el campo de los granitos tipo I, y a la unidad Intrusivo Gnéisico como granito tipo S. Todos presentan firmas químicas de Rb, Y y Nb típicas de granitoides de subducción, de serie calcoalcalina y tipo magnésicos. Dataciones U-Pb mediante LA-ICP-MS en circones arrojaron edades de 132,8±2,6 Ma para la Alaskita de Samaná, 129,8±9,7 Ma para el Complejo Ígneo de Samaná, 54,6±4,4 Ma para el Stock de Florencia y 47±11 Ma para el Batolito de Sonsón. Nueve cuerpos porfiríticos andesiticos (Pl+Anf) de los cuales cinco fueron reconocidos en las labores de campo de este trabajo, se expresan algunos de ellos con evidentes formas dómicas y matrices vítreas. Estos cuerpos porfiríticos presentan mayor grado de alteración hidrotermal (fílica y argílica) en especial en el sector de Puente Linda, controlados estructuralmente, con presencia de brechas orientadas este-oeste a lo largo del rio Samaná. Todos estos cuerpos con firmas adakiticas (Sr entre 335,31 y 1160,25 ppm) presentan anomalía positiva de EuN/&#8730;(SmN *Gd N) desde 1,34 a 2,07. El pórfido de Puente Linda (Pl + Qz + Anf ± Cb ± K ± Dck) tiene sobreimpuesta la mayor alteración en extensión y grado; datación U-Pb arrojó una edad de 2,1±1,9 Ma. Por otro lado, cinco cuerpos aflorantes de naturaleza dacítica (Qz + Pl + Anf) fueron reconocidos y caracterizados, cuya geoquímica contrastante con las demás intrusiones, presentando anomalías negativas de EuN/&#8730;(SmN *Gd N) desde 0,18 a 0,64. Finalmente, dos estructuras volcánicas, domo de San Diego (Qz + Pl + Bt) y Domos del volcán El Escondido (Pl + Anf) se reconocen como evidencias de actividad volcánicas reciente; dataciones Ar-Ar registraron una edad Plateau de 89±4,4 Ka para San Diego y de 153,7±38,2 Ka para El Escondido.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Five plutonic bodies were characterized in the San Diego geothermal area, whose chemical characteristics position four units (Florencia Stock, Sonsón Batholith, Samaná Complex and Samaná Alaskite) in the field of granites type I, and the Gneissic Intrusive as granite type S. All have chemical signatures of Rb, Y and Nb typical of subduction environment granitoids, calcoalcaline series and magnesium type. The U-Pb data by LA-ICP-MS in zircons showed ages of 132.8±2.6 my for the Samaná Alaskite, 129.8±9.7 my for the Samaná Igneous Complex, 54.6±4.4 my for the Florencia Stock and 47±11 my for the Sonsón Batholith. Nine andesitic porphyritic bodies (Pl+Anf) of which five were recognized in this work, are expressed some of them with evident domic forms and vitreous matrices. These porphyritic bodies present a greater degree of hydrothermal alteration (phyllic and argillic), especially in the Puente Linda sector, structurally controlled, with the presence of oriented breccias (EW) along the Samaná River. All of these bodies with adakitic signatures (Sr between 335.31 and 1160.25 ppm) have positive anomaly EuN/&#8730;(SmN *Gd N) from 1.34 to 2.07. The Puente Linda porphyry (Pl + Qz + Anf ± Cb ± K ± Dck) has superimposed the greater alteration in extension and degree; U-Pb dating in zircons, showed an age of 2.1±1.9 Ma. On the other hand, five dacite bodies (Qz + Pl + Anf) were equally recognized and characterized, whose geochemistry contrasted with that of other intrusions, with negative anomalies EuN/&#8730;(SmN *Gd N) from 0.18 to 0.64. Finally, two volcanic structures, San Diego dome (Qz + Pl + Bt) and El Escondido volcano domes (Pl + Anf) are recognized as evidence of recent volcanic activity; Ar-Ar dating recorded a Plateau age of 89±4.4 Ka for San Diego and 153.7±38.2 Ka for El Escondido.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[San Diego]]></kwd>
<kwd lng="es"><![CDATA[geotermia]]></kwd>
<kwd lng="es"><![CDATA[dataciones U-Pb]]></kwd>
<kwd lng="es"><![CDATA[dataciones Ar-Ar]]></kwd>
<kwd lng="es"><![CDATA[geoquímica.]]></kwd>
<kwd lng="en"><![CDATA[San Diego]]></kwd>
<kwd lng="en"><![CDATA[geothermal]]></kwd>
<kwd lng="en"><![CDATA[U-Pb dating]]></kwd>
<kwd lng="en"><![CDATA[Ar-Ar dating]]></kwd>
<kwd lng="en"><![CDATA[geochemistry.]]></kwd>
</kwd-group>
</article-meta>
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