<?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>S0120-02832023000100015</article-id>
<article-id pub-id-type="doi">10.18273/revbol.v45n1-2023001</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[The relation between monogenetic and polygenetic dacitic volcanism. Case study from Tapias dome (&lt;95 ka) and Cerro Machín volcano (&lt;50 ka), Colombia]]></article-title>
<article-title xml:lang="es"><![CDATA[Relación entre vulcanismo dacítico monogenético y poligenético. Caso de estudio del domo Tapias (&lt;95 ka) y volcán Cerro Machín (&lt;50 ka), Colombia]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortiz]]></surname>
<given-names><![CDATA[Jonathan]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García]]></surname>
<given-names><![CDATA[Jhoan Sebastián]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Murcia]]></surname>
<given-names><![CDATA[Hugo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Schonwalder-Ángel]]></surname>
<given-names><![CDATA[Dayana]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez-Torres]]></surname>
<given-names><![CDATA[Laura]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Caldas Programa de Geología ]]></institution>
<addr-line><![CDATA[Manizales ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Caldas Programa de Geología ]]></institution>
<addr-line><![CDATA[Manizales ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Caldas Departamento de Ciencias Geológicas ]]></institution>
<addr-line><![CDATA[Manizales ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad de Caldas Grupo de Investigación en Estratigrafía y Vulcanología (GIEV) Cumanday ]]></institution>
<addr-line><![CDATA[Manizales ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Universidad de Caldas Instituto de Investigaciones en Estratigrafía ]]></institution>
<addr-line><![CDATA[Manizales ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>04</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>04</month>
<year>2023</year>
</pub-date>
<volume>45</volume>
<numero>1</numero>
<fpage>15</fpage>
<lpage>35</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0120-02832023000100015&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0120-02832023000100015&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0120-02832023000100015&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Tapias lava dome is located ~5 km SE of the explosive, Cerro Machín polygenetic volcano, both located on the Colombian Central Cordillera. The edifices have been interpreted as generated by the same magmatic system; however, the genetic and temporal relations between both edifices have not been established. In this work, the Tapias dome is studied using petrographic characterizations, mineral-, whole-rock- and isotopic chemistry, geothermobarometric calculations, and a K/Ar radiogenic age, and subsequently it is explored the relationship with the Cerro Machín. The rocks from Tapias dome are porphyritic with phenocrysts of plagioclase (An28-48), amphibole (tschermakite and magnesiohastingsite), biotite, quartz, and Fe-Ti oxides, embedded in a glassy groundmass. Petrographically, two types of amphibole crystals were recognized: type I, which is homogeneous, and type II, which displays different rims. The composition of Tapias is dacitic (SiO2: 66.59 wt.%) with calc-alkaline affinity. Our geothermobarometric calculations indicate that type I amphibole crystallized at 871-874°C, between 10.2 and 10.4 km depth. The core of the type II amphibole crystallized at 852-920°C, between 8.5 and 12.3 km depth, while its rim did it at higher temperatures (880-973°C), but at similar depths (9.1-11.8 km). The K/Ar radiogenic age obtained for the groundmass shows an emplacement age not older than 95 ± 0.05 ka. When comparing the results to the Cerro Machín, it is noted that the mineral and compositional characteristics are nearly identical. These results suggest that indeed both volcanoes share the same magmatic system and are fed by magma hosted between ~9 and ~12 km depth. Moreover, it is proposed that the vent location of both edifices, as well as the time gap between the eruption at Tapias and the beginning of the activity at the Cerro Machín (~50 ka), are the result of crustal deformation caused by the interaction between the Otú-Pericos and Ibagué faults.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El domo Tapias es un edificio volcánico que se localiza ~5 km al SE del volcán poligenético explosivo Cerro Machín, ambos localizados en la Cordillera Central colombiana. La formación de estos volcanes ha sido interpretada a partir del mismo sistema magmático; sin embargo, la relación genética y temporal entre ellos no ha sido definida. En este trabajo, se analiza el domo Tapias a partir de petrografía, química mineral, química de roca total, isótopos, cálculos geotermobarométricos y una datación K/Ar, y posteriormente se explora la relación con el volcán Cerro Machín. Las rocas del domo Tapias son porfiríticas con fenocristales de plagioclasa (An28-48), anfíbol (tschermakita y magnesiohastingsita), biotita, cuarzo y óxidos de Fe-Ti, embebidos en una masa fundamental vítrea. Petrográficamente, se reconocen dos tipos de anfíbol: el tipo I, con apariencia homogénea, y el tipo II, con bordes diferentes. La composición de Tapias es dacítica (SiO2: 66,59 wt.%) de afinidad calco-alcalina. Los cálculos geotermobarométricos indican que: 1) los anfíboles tipo I cristalizaron a 871-874°C, entre 10,2 y 10,4 km de profundidad, y 2) los núcleos de los anfíboles tipo II cristalizaron a 852-920°C, entre 8,5 y 12,3 km de profundidad, mientras que los bordes, a temperaturas más altas (880-973°C), pero a profundidades similares (9,1-11,8 km). La edad K/Ar indica un emplazamiento no más antiguo que 95 ± 0,05 ka. Al comparar estos resultados con los reportados para el Cerro Machín, se observan unas características minerales y composicionales muy similares. Estos resultados sugieren que ambos volcanes son alimentados por el mismo magma hospedado entre ~9 y ~12 km de profundidad. Asimismo, se propone que el centro de emisión, así como el tiempo entre el emplazamiento de Tapias y el inicio de la actividad del Cerro Machín (~50 ka) son el resultado de deformación cortical relacionada con la interacción entre las fallas Otú-Pericos e Ibagué.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Monogenetic volcanism]]></kwd>
<kwd lng="en"><![CDATA[Magma differentiation]]></kwd>
<kwd lng="en"><![CDATA[Local tectonics]]></kwd>
<kwd lng="en"><![CDATA[Colombian Andes]]></kwd>
<kwd lng="es"><![CDATA[Vulcanismo monogenético]]></kwd>
<kwd lng="es"><![CDATA[Diferenciación magmática]]></kwd>
<kwd lng="es"><![CDATA[Tectónica local]]></kwd>
<kwd lng="es"><![CDATA[Andes colombianos]]></kwd>
</kwd-group>
</article-meta>
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