Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy

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Fecha de publicación:: 2025

Institución:: Universidad de Caldas

Repositorio:: Repositorio Institucional U. Caldas

Idioma:: spa

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network_acronym_str	REPOUCALDA
network_name_str	Repositorio Institucional U. Caldas
repository_id_str
dc.title.none.fl_str_mv	Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy
title	Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy
spellingShingle	Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy 550 - Ciencias de la tierra 1. Ciencias Naturales Monogenético Evolución magmática Litósfera-Astenósfera Zona de subducción Cristalización fraccionada Geotermobarometría Vulcanología Geología
title_short	Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy
title_full	Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy
title_fullStr	Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy
title_full_unstemmed	Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy
title_sort	Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy
dc.contributor.none.fl_str_mv	Murcia Agudelo, Hugo Fernando Sánchez Torres, Laura Universidad de Caldas GIEV-(CUMANDAY) Grupo de Investigación en Estratigrafía y Vulcanología (Categoría A1) Jaimes-Viera, Carmen Ureta, Gabriel
dc.subject.none.fl_str_mv	550 - Ciencias de la tierra 1. Ciencias Naturales Monogenético Evolución magmática Litósfera-Astenósfera Zona de subducción Cristalización fraccionada Geotermobarometría Vulcanología Geología
topic	550 - Ciencias de la tierra 1. Ciencias Naturales Monogenético Evolución magmática Litósfera-Astenósfera Zona de subducción Cristalización fraccionada Geotermobarometría Vulcanología Geología
description	tablas, figuras
publishDate	2025
dc.date.none.fl_str_mv	2025-05-14T14:25:26Z 2025-05-14T14:25:26Z 2025-05-13
dc.type.none.fl_str_mv	Trabajo de grado - Maestría Text info:eu-repo/semantics/masterThesis http://purl.org/redcol/resource_type/TM
dc.identifier.none.fl_str_mv	https://repositorio.ucaldas.edu.co/handle/ucaldas/22206 Universidad de Caldas Repositorio Institucional Universidad de Caldas repositorio.ucaldas.edu.co
url	https://repositorio.ucaldas.edu.co/handle/ucaldas/22206
identifier_str_mv	Universidad de Caldas Repositorio Institucional Universidad de Caldas repositorio.ucaldas.edu.co
dc.language.none.fl_str_mv	spa
language	spa
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dc.publisher.none.fl_str_mv	Universidad de Caldas Facultad de Ciencias Exactas y Naturales Manizales, Caldas, Colombia Maestría en Ciencias de la Tierra
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spelling	Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy550 - Ciencias de la tierra1. Ciencias NaturalesMonogenéticoEvolución magmáticaLitósfera-AstenósferaZona de subducciónCristalización fraccionadaGeotermobarometríaVulcanologíaGeologíatablas, figurasEl Campo Volcánico Monogenético Guamuez-Sibundoy está ubicado en el Segmento Volcánico Sur, en la Cordillera Central de Colombia. Este campo alberga al menos 19 volcanes, desde conos de escoria y maares hasta domos de lava. Este tipo de vulcanismo hace parte del arco volcánico ocasionado por la interacción entre la placa Nazca y Suramericana y un ambiente tectónico transtensional con formación de cuencas pull-apart y fallas regionales asociadas al Sistema de Fallas Algeciras que permitieron el emplazamiento de los volcanes. Este estudio integra técnicas de geología de campo, petrografía, química mineral, química de roca total y análisis geotermobarométricos con el fin de conocer las características composicionales y reconstruir la evolución de los magmas que dieron origen a algunos volcanes. Los productos asociados a los volcanes en estudio (Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy) corresponden a corrientes de densidad piroclástica concentradas y diluidas y flujos de lava, estos últimos predominando en todo el campo. Mineralógicamente todas las rocas están compuestas por olivino (Fo71-90), clinopiroxeno (Wo33-48, En36-54, Fe7-16) y plagioclasa (An26-82), además de ortopiroxeno (Wo3-5, En68-71, Fe24-28) solamente en el volcán Fuisanoy y anfíbol (magnesiohastingsita y tschermakita) exclusivamente en los volcanes Yaku y Mujundinoy Sur. Óxidos de Fe-Ti están presentes como fase menor en todos los volcanes. Petrográficamente, las rocas son porfiríticas, con textura fluidal y seriada, masa fundamental microcristalina, criptocristalina y vítrea; también presentan textura glomeroporfirítica en olivino,clinopiroxeno y ortopiroxeno, zonación normal en plagioclasa, esqueletal en olivino y clinopiroxeno y textura spinifex en clinopiroxeno. Químicamente, los volcanes son de composición basáltica y andesita basáltica, de afinidad calco-alcalina media en potasio, típico de ambientes de subducción. Análisis geotermobarométricos indican que las condiciones de cristalización para el olivino fueron de 1188 – 1137 °C, para el clinopiroxeno de 1199 – 1015 °C y 1,7 – 0,2 GPa y para la plagioclasa de 1127 – 1077 °C y 0,6 – 0,2 GPa. Todos estos análisis permiten evidenciar que los magmas comparten un origen común en el límite astenósfera-litósfera y que el proceso de evolución magmática más importante fue la cristalización fraccionada durante el ascenso e incluso durante cortos periodos de estancamiento en la corteza. Las altas temperaturas para el olivino podrían indicar cristalización en límite manto-corteza o incluso a mayor profundidad, aunque no se obtuvieron datos de presión para esta fase. Las condiciones de cristalización de las fases minerales indican que el clinopiroxeno fue el primero en cristalizar en el límite manto-corteza aunque se mantuvo hasta niveles corticales (64 – 7 km), seguido por la cristalización de plagioclasa solamente a niveles corticales (24 – 7 km). Datos químicos y condiciones de cristalización indican que el volcán Guayapungo ascendió directamente desde el manto y experimentó un ascenso rápido desde los 15 km hasta la superficie. Ausencia de cristalización de los minerales, así como xenocristales de anfíbol y condiciones anómalas de cristalización de esta fase mineral (903 °C y 1,7 GPa), indican que los magmas de los volcanes Yaku y Mujundinoy Sur experimentaron leve asimilación cortical. Condiciones de cristalización y mayor evolución en el volcán Fuisanoy indican que este volcán pudo haber tenido un ascenso más lento. Finalmente, un depósito de caída de 17 ka que cubre los volcanes, marca el límite temporal mínimo de la última erupción.The Guamuez-Sibundoy Monogenetic Volcanic Field is located in the Southern Volcanic Segment of the Central Cordillera of Colombia. This field hosts 19 volcanoes, which has been defined as scoria cones, maars and lava domes. This type of volcanism is part of the volcanic arc caused by the interaction between the Nazca and South American plates and a transtensional tectonic environment with the formation of pull-apart basins and regional faults associated with the Algeciras Fault System. This study integrates field geology, petrography, mineral chemistry, whole-rock chemistry and geothermobarometric analysis techniques in order to know the compositional characteristics and reconstruct the evolution of the magmas that gave rise to 4 of the 19 volcanoes in the field: Guayapungo, Yaku, Mujundinoy Sur and Fuisanoy volcanoes. The products associated with these volcanoes correspond to concentrated and dilute pyroclastic density currents and lava flows, the latter predominating throughout the field. Mineralogically, all rocks are composed of olivine (Fo71-90), clinopyroxene (Wo33-48, En36-54, Fe7-16) and plagioclase (An26-82), plus orthopyroxene (Wo3-5, En68-71, Fe24-28) only in Fuisanoy volcano and amphibole (magnesiohansgtinsite and tschermakite) exclusively in Yaku and Mujundinoy Sur volcanoes. Petrographically, the rocks are porphyritic, with olivine, clinopyroxene, orthopyroxene, plagioclase, amphibole and Fe-Ti oxides as mineral phases embedded in a microcrystalline, cryptocrystalline and glassy groundmass. They present glomeroporphyritic texture in olivine and pyroxene, zoning in plagioclase, skeletal in olivine and pyroxene, and spinifex texture in pyroxene. Fluidal and serial texture is also common. Fe-Ti oxides are present as a minor phase in all volcanoes. Chemically, the volcanics are basaltic and basaltic andesite in composition, and display calc-alkaline affinity, typical of subduction environments. Geothermobarometric analyses indicate that the crystallization conditions for olivine were 1188 – 1137 °C, for clinopyroxene 1199 – 1015 °C and 1.7 – 0.2 GPa and for plagioclase 1127 – 1077 °C and 0.6 – 0.2 GPa. The analyses indicate that the magmas share a common origin at the asthenosphere-lithosphere boundary and that fractional crystallization was the most important magmatic evolution process during ascent. The crystallisations conditions of the mineral phases indicate that olivine, followed by clinopyroxene, were the first to crystallise at the mantle-crust boundary (or below) and it remained until cortical levels (64 – 7 km); plagioclase crystallised only at cortical levels (24 – 7 km). Chemical data and crystallisation conditions indicate that the Guayapungo volcano ascended directly from the mantle and experienced a rapid ascent from 15 km to the surface. Absence of mineral crystallization, in addition to the presence of amphibole xenocrysts and anomalous crystallization conditions of this mineral phase (800 °C and 1.7 GPa), indicate that the Yaku and Mujundinoy Sur magmas experienced mild assimilation. Crystallisation conditions and further evolution at Fuisanoy volcano indicate that this volcano may have had a slower ascent.Introducción -- Objetivos -- Marco geológico -- Campo Volcánico Monogenético Guamuez-Sibundoy -- Geología estructural y tectónica -- Metodología -- Trabajo de campo y recolección de muestras -- Petrografía -- Química mineral -- Química de roca total -- Marco teórico -- Vulcanismo monogenético -- Estilos eruptivos en vulcanismo monogenético -- Sistemas magmáticos en vulcanismo monogenético -- Procesos de evolución magmática -- Resultados -- Volcanes y sus productos -- Volcán Guayapungo -- Volcán Yaku -- Volcán Mujundinoy Sur --Volcán Fuisanoy -- Petrografía -- Volcán Guayapungo -- Volcán Yaku -- Volcán Mujundinoy Sur -- Volcán Fuisanoy -- Química mineral -- Volcán Guayapungo -- Volcán Yaku -- Volcán Mujundinoy Sur -- Volcán Fuisanoy -- Química de roca total -- Discusión -- Análisis textural -- ¿Textura Spinifex? -- Geotermobarometría --Olivino -- Clinopiroxeno -- Plagioclasa -- Anfíbol -- Óxidos de Fe-Ti -- Evolución magmática -- Fusión parcial -- Cristalización fraccionada -- ¿Asimilación cortical o fraccionamiento de anfíbol? -- Modelo de evolución magmática del CVMGS -- Implicaciones de amenaza volcánica -- Conclusiones -- ReferenciasMaestríaPara este estudio se realizó una campaña de campo de 10 días con el fin de reconocer las estructuras del CVMGS, correlacionar estratigráficamente sus depósitos y reconocer geoformas asociadas a los volcanes Guayapungo, Yaku, Mujudinoy Sur y Fuisanoy. Se hicieron recorridos estratégicos con el fin de realizar un mapeo, tomar puntos de control y recolectar muestras de roca fresca, correlacionables con afloramientos de cada volcán, de aproximadamente 1000 g cada una. En total se recolectaron 10 muestras, una perteneciente a una bomba volcánica y nueve a flujos de lava. De estas, cuatro son del volcán Guayapungo, una de Yaku, dos de Mujundinoy Sur y tres de Fuisanoy. El número de muestras varía de acuerdo con las condiciones de acceso a cada volcán, el estado de las rocas aflorantes y la disponibilidad de estas para el muestreo. Para el análisis petrográfico se realizaron 10 secciones delgadas pulidas, una de cada muestra recolectada en campo, en los laboratorios de TecLab en Bogotá (Colombia). Posteriormente, las secciones se analizaron a través de un microscopio Nikon Eclipse E200 en el laboratorio de petrografía del Instituto de Investigaciones en Estratigrafía (IIES) de la Universidad de Caldas (Colombia); así, se definieron las asociaciones mineralógicas y las texturas de los minerales. El tamaño de los cristales fue definido de acuerdo con González (2008) dónde los fenocristales son > 0,5 mm, los microfenocristales entre 0,5 – 0,05 mm y microcristales son < 0,05 mm y hacen parte de la masa fundamental. Las abreviaciones de los nombres de los minerales se tomaron de Whitney & Evans (2010): olivino (Ol), piroxeno (Px), plagioclasa (Pl) y anfíbol (Anf). Finalmente, se marcaron puntos de interés sobre la sección para posterior análisis de química mineral.Magister en Ciencias de la TierraVulcanologíaUniversidad de CaldasFacultad de Ciencias Exactas y NaturalesManizales, Caldas, ColombiaMaestría en Ciencias de la TierraMurcia Agudelo, Hugo FernandoSánchez Torres, LauraUniversidad de CaldasGIEV-(CUMANDAY) Grupo de Investigación en Estratigrafía y Vulcanología (Categoría A1)Jaimes-Viera, CarmenUreta, GabrielToro Agudelo, Ana María2025-05-14T14:25:26Z2025-05-14T14:25:26Z2025-05-13Trabajo de grado - MaestríaTextinfo:eu-repo/semantics/masterThesishttp://purl.org/redcol/resource_type/TM150 páginasapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttps://repositorio.ucaldas.edu.co/handle/ucaldas/22206Universidad de CaldasRepositorio Institucional Universidad de Caldasrepositorio.ucaldas.edu.cospaAbdel-Rahman, A. F. M., & Nassar, P. E. (2004). Cenozoic volcanism in the Middle East: petrogenesis of alkali basalts from northern Lebanon. 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Evolución magmática en el Campo Volcánico Monogenético Guamuez-Sibundoy (Colombia) a partir del estudio de los volcanes Guayapungo, Yaku, Mujundinoy Sur y Fuisanoy

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