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Condiciones de cristalización de los volcanes Tesorito, Gallinazo y Victoria, Campo Volcánico Monogenético Villamaría-Termales, Colombia
dc.contributor.advisor | Murcia Agudelo, Hugo Fernando | spa |
dc.contributor.author | Salazar Muñoz, Natalia | spa |
dc.contributor.author | Rios de la Ossa, Carlos Arturo | spa |
dc.date.accessioned | 2020-08-27T23:51:16Z | spa |
dc.date.available | 2020-08-27T23:51:16Z | spa |
dc.date.issued | 2019-10-29 | spa |
dc.identifier.uri | https://repositorio.ucaldas.edu.co/handle/ucaldas/7763 | spa |
dc.description | 117 hojas | spa |
dc.description.abstract | spa: El vulcanismo monogenético hace referencia a discretos eventos de salida de magma a superficie y que por definición forman volcanes a partir de una sola erupción. Estos volcanes normalmente aparecen en grupo durante un tiempo y un área definida, formando de esta manera campos volcánicos monogenéticos. El denominado Campo Volcánico Monogenético Villamaría-Termales (CVMVT) es una expresión de este vulcanismo (14 volcanes tipo domos de lava), localizado en el flanco occidental de la Cordillera Central de Colombia. Este trabajo presenta una caracterización petrográfica y química de tres domos de lava: Victoria, Gallinazo y Tesorito, con el objetivo de evaluar las condiciones de cristalización de estos productos eruptivos. Mineralógicamente, estos volcanes están compuestos de plagioclasa (An31-67), piroxeno (Wo2-45 – En39-80 – Fs8-32) y anfíbol. Olivino (Fo71-87) solo es reconocido en el domo Victoria. Químicamente, los volcanes presentan composición andesítica y una firma calcoalcalina alta en K, además de una firma adakítica. Los resultados geotermobarométricos revelan que el olivino fue la primera fase mineral en cristalizar (1215 – 1228 °C) para el magma alimentador del domo Victoria, seguido del ortopiroxeno (1062 – 1067 °C), clinopiroxeno (1026 – 1056 °C), plagioclasa (905 – 1045 °C) y anfíbol (~987 °C). En el domo Gallinazo, el orden de cristalización fue: ortopiroxeno (1050 – 1076 °C), clinopiroxeno (972 – 1025 °C), plagioclasa (900 – 1044 °C) y anfíbol (899 – 964 °C); y para el domo Tesorito el orden de cristalización fue: ortopiroxeno (1138 – 1145 °C), clinopiroxeno (1009 – 1038 °C), plagioclasa (894 – 1050 °C) y anfíbol (921 – 974 °C). En general, las presiones estimadas indican que los procesos de cristalización empezaron a 1.5 GPa y continuaron hasta que el material alcanzó superficie. Estos valores sugieren que la cristalización de las fases minerales de cada domo se dio en numerosas zonas de estancamiento ubicadas a lo largo de los conductos por el cual ascendió el magma. El análisis de microtexturas en plagioclasa y las características del vidrio de cada domo sugieren procesos de cristalización fraccionada y contaminación cortical durante la cristalización del magma. Las características geoquímicas del CVMVT permiten identificar una relación genética con los volcanes poligenéticos Cerro Bravo y Nevado del Ruiz. | spa |
dc.description.abstract | eng: Monogenetic volcanism refers to discrete events of magma extrusion forming volcanoes in a single eruption. Clusters of these volcanoes, localised in a defined time and area, form monogenetic volcanic fields. The so-called Villamaría-Termales Monogenetic Volcanic Field (CVMVT) is an expression of this volcanism (14 lava dome types), which is located on the western flank of the Central Cordillera of Colombia. This work presents a petrographic and chemical characterisation of three lava domes: Victoria, Gallinazo and Tesorito, with the objective of evaluating the crystallisation conditions of these eruptive products. Mineralogically, these volcanoes are composed of plagioclase (An31-67), pyroxene (Wo2-45 – En39-80 – Fs8-32) and amphibole. Olivine (Fo71-87) was only recognised on the Victoria dome. Chemically, the volcanoes have an andesitic composition and a high K calc-alkaline signature, in addition to an adakitic signature. The geothermobarometric results indicate that olivine (1215 – 1228 °C) was the first mineral phase to crystallise in the Victoria dome feeding magma, followed by orthopyroxene (1062 – 1067 °C), clinopyroxene (1026 – 1056 °C), plagioclase (905 – 1045 °C) and amphibole (~ 987 °C). In the Gallinazo dome, the order of crystallisation was: orthopyroxene (1050 – 1076 °C), clinopyroxene (972 – 1025 °C), plagioclase (900 – 1044 °C) and amphibole (899 – 964 °C); and for the Tesorito dome the order of crystallisation was: orthopyroxene (1138 – 1145 °C), clinopyroxene (1009 – 1038 °C), plagioclase (894 – 1050 °C) and amphibole (921 – 974 °C). The estimated pressures indicate that the crystallisation processes started at 1.5 GPa and continued until the magma reached surface. These values suggest that the crystallisation of the mineral phases of each dome occurred in numerous areas of stagnation located along the magma conduits. The analysis of micro-textures in plagioclase and the characteristics of the glass suggest processes of fractional crystallisation and cortical contamination during the magma ascent. Geochemical characteristics of the CVMVT allow evidencing a genetic relationship with the polygenetic volcanoes Cerro Bravo and Nevado del Ruiz. | spa |
dc.description.tableofcontents | 1. INTRODUCCIÓN / 2. OBJETIVOS / 2.1 OBJETIVO GENERAL / 2.2 OBJETIVOS ESPECÍFICOS / 3. MARCO GEOLÓGICO / 3.1 CAMPO VOLCÁNICO MONOGENÉTICO VILLAMARÍA-TERMALES / 4. MARCO TEÓRICO / 4.1 VULCANISMO MONOGENÉTICO / 4.2 VOLCANES MONOGENÉTICOS FORMADOS POR ERUPCIÓN MAGMÁTICA /4.2.1 Conos de escoria / 4.2.2 Domos de lava / 4.2.3 Flujos de lava / 4.3 VOLCANES MONOGENÉTICOS FORMADOS POR ERUPCIÓN FREATO-MAGMÁTICA / 4.3.1FUNDAMENTACIÓN BIBLIOGRÁFICA Conos de toba / 4.3.2 Anillos de toba / 4.3.3 Maares / 5. METODOLOGÍA / 5.1 / FUNDAMENTACIÓN BIBLIOGRÁFICA /5.2 TRABAJO DE CAMPO Y MUESTREO / 5.3 ANÁLISIS PETROGRÁFICO / 5.4 ANÁLISIS QUÍMICOS / 5.4.1 Química mineral / 5.4.2 Química de roca total / 6. RESULTADOS / PETROGRAFÍA / 6.1.1 Domo Victoria / 6.1.2 Domo Gallinazo / 6.1.3 Domo Tesorito / 6.2 QUÍMICA MINERAL / 6.2.1 Olivino / 6.2.2 Piroxeno / 6.2.3 Plagioclasa / 6.2.4 Anfíbol / 6.2.5 Óxido de Fe-Ti / 6.2.6 Vidrio / 6.3 QUÍMICA DE ROCA TOTAL / 7. DISCUSIÓN / 7.1 TEXTURAS EN PLAGIOCLASA / 7.2 VIDRIO VOLCÁNICO / 7.3 GEOTERMOBAROMETRÍA / 7.3.1 Olivino / 7.3.2 Ortopiroxeno / 7.3.3 Clinopiroxeno / 7.3.4 Plagioclasa / 7.3.5 Anfíbol / 7.4 MODELO PETROGENÉTICO / 7.4.1 Domo Victoria / 7.4.2 Domo Gallinazo / 7.4.3 Domo Tesorito / 7.5 COMPARACIÓN CON LOS OTROS CAMPOS VOLCÁNICOS MONOGENÉTICOS DE LA PROVINCIA VOLCANO-TECTÓNICA SAN DIEGO – CERRO MACHÍN (PVTSC)/ 7.6 COMPARACIÓN EL CAMPO VOLCÁNICO MOGENÉTICO VILLAMARÍA-TERMALES (CVMVT), VOLCÁN NEVADO DEL RUIZ Y VOLCÁN CERRO BRAVO / 7.7 ADAKITAS / 8. CONCLUSIONES /9. REFERENCIAS BIBLIOGRÁFICAS | spa |
dc.format.mimetype | application/pdf | spa |
dc.language.iso | eng | spa |
dc.language.iso | spa | spa |
dc.rights | Copyright (c) 2020 Universidad de Caldas | spa |
dc.rights.uri | https://creativecommons.org/licenses/by-nc/4.0/ | spa |
dc.title | Condiciones de cristalización de los volcanes Tesorito, Gallinazo y Victoria, Campo Volcánico Monogenético Villamaría-Termales, Colombia | spa |
dc.type | Trabajo de grado - Pregrado | spa |
dc.contributor.educationalvalidator | Schonwalder Angel, Dayana | spa |
dc.description.degreelevel | Universitario | spa |
dc.identifier.instname | Universidad de Caldas | spa |
dc.identifier.local | T06019044 / S161 | spa |
dc.identifier.reponame | Repositorio Institucional Universidad de Caldas | spa |
dc.identifier.repourl | https://repositorio.ucaldas.edu.co/ | spa |
dc.publisher.faculty | Facultad de Ciencias Exactas y Naturales | spa |
dc.publisher.place | Manizales | spa |
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dc.rights.accessrights | info:eu-repo/semantics/closedAccess | spa |
dc.rights.creativecommons | Atribución-NoComercial | spa |
dc.subject.proposal | Vulcanismo monogenético | spa |
dc.subject.proposal | Química mineral | spa |
dc.subject.proposal | Geotermobarometría | spa |
dc.subject.proposal | Domo de lava | spa |
dc.subject.proposal | Monogenetic volcanism | spa |
dc.subject.proposal | Mineral chemistry | spa |
dc.subject.proposal | Geothermobarometry | spa |
dc.subject.proposal | Lava dome | spa |
dc.subject.proposal | Vulcanismo monogenético | spa] |
dc.subject.proposal | Química mineral | spa] |
dc.subject.proposal | Geotermobarometría | spa] |
dc.subject.proposal | Domo de lava | spa] |
dc.subject.proposal | Monogenetic volcanism | spa] |
dc.subject.proposal | Mineral chemistry | spa] |
dc.subject.proposal | Geothermobarometry | spa] |
dc.subject.proposal | Lava dome | spa] |
dc.type.coar | http://purl.org/coar/resource_type/c_7a1f | spa |
dc.type.content | Text | spa |
dc.type.driver | info:eu-repo/semantics/bachelorThesis | spa |
dc.type.redcol | https://purl.org/redcol/resource_type/TP | spa |
dc.type.version | info:eu-repo/semantics/acceptedVersion | spa |
oaire.version | http://purl.org/coar/version/c_b1a7d7d4d402bcce | spa |
oaire.accessrights | http://purl.org/coar/access_right/c_14cb | spa |
dc.description.degreename | Geólogo(a) | spa |
dc.publisher.program | Geología | spa |
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