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| Campo DC | Valor | Lengua/Idioma |
|---|---|---|
| dc.contributor.author | Hernández Villamizar, Daniela. | - |
| dc.date.accessioned | 2026-10-16T02:16:55Z | - |
| dc.date.available | 2024 | - |
| dc.date.available | 2026-10-16T02:16:55Z | - |
| dc.date.issued | 2024 | - |
| dc.identifier.citation | Hernández Villamizar, D. Y. (2024). Morfología y reología cuantitativa de la fase efusiva de los volcanes monogenéticos Melón, Mina, Tzinzimacato grande y Tzinzimacato Chico, localizados al occidente de la ciudad de Morelia, México. [Trabajo de Grado Pregrado, Universidad de Pamplona]. Repositorio Hulago Universidad de Pamplona. https://repositoriodspace.unipamplona.edu.co/jspui/handle/20.500.12744/11804 | es_CO |
| dc.identifier.uri | https://repositoriodspace.unipamplona.edu.co/jspui/handle/20.500.12744/11804 | - |
| dc.description | Cuatro volcanes monogenéticos se formaron durante los últimos 100 ka (Pleistoceno-Tardío), al occidente de la ciudad de Morelia (México), en la parte centro-oriental del Campo Volcánico Michoacán-Guanajuato, situado en la región central del Cinturón Volcánico Transmexicano. Estos incluyen cuatro conos de escoria (Melón, Mina, Tzinzimacato Grande y Tzinzimacato Chico) y varios depósitos de flujos de lava asociados al material emitido durante su fase efusiva. A partir del estudio de las relaciones estratigráficas en campo y el mapeo geológico, se determinó la cronología eruptiva. Posteriormente con base en el análisis de las características morfológicas (dimensiones de flujo) y petrográficas se estimaron los parámetros eruptivos (tasa de efusión y tiempo de la erupción), y la reología de las lavas. Los resultados indican que las lavas más viscosas corresponden a las emitidas por los volcanes Tzinzimacato Grande y Chico; 7.35X109-2.89X109 Pa·s respectivamente, con temperaturas promedio entre 1061-1115 C°. La erupción más voluminosa fue la emitida por el volcán Mina, con una tasa de efusión de 2.4 m3/s y una duración total aproximada de 1.5 años. Aunque el volumen total emitido por el volcán Melón no es tan grande, los datos arrojaron una tasa de efusión alta, lo que probablemente se debe a la composición más máfica de sus lavas. | es_CO |
| dc.description.abstract | Four monogenetic volcanoes erupted during the last 100 ka (Late-Pleistocene), west of the city of Morelia (Mexico), in the central-eastern part of the Michoacán-Guanajuato Volcanic Field, located in the central region of the Trans-Mexican Volcanic Belt. These include four scoria cones (Melón, Mina, Tzinzimacato Grande and Tzinzimacato Chico) including lava flows associated with the material emitted during their effusive phase. From the study of stratigraphic relationships in the field and geological mapping, the eruptive chronology was determined. Subsequently, based on the analysis of the morphological (flow dimensions) and petrographic characteristics, the eruptive parameters (effusion rate and eruption time) and the rheology of the lavas were estimated. The results indicate that the most viscous lavas were those emitted by the Tzinzimacato Grande and Chico volcanoes; 7.35x109-2.89x109 Pa-s respectively, at average temperatures of 1061-1115 C°, the most voluminous eruption was the one emitted the Mina volcano, with an effusion rate of 2.4 m3/s and a total duration of approximately 1.5 years. Although the total volume emitted by Melón volcano is not as large, the data revealed a high effusion rate, probably due to a more mafic composition of its lavas. | es_CO |
| dc.format.extent | 24 | es_CO |
| dc.format.mimetype | application/pdf | es_CO |
| dc.language.iso | es | es_CO |
| dc.publisher | Universidad de Pamplona - Facultad de Ciencias Básicas. | es_CO |
| dc.subject | Volcán monogenético. | es_CO |
| dc.subject | Morfología. | es_CO |
| dc.subject | Reología. | es_CO |
| dc.subject | Temperatura. | es_CO |
| dc.subject | Flujos de lava. | es_CO |
| dc.title | Morfología y reología cuantitativa de la fase efusiva de los volcanes monogenéticos Melón, Mina, Tzinzimacato grande y Tzinzimacato Chico, localizados al occidente de la ciudad de Morelia, México. | es_CO |
| dc.type | http://purl.org/coar/resource_type/c_7a1f | es_CO |
| dc.date.accepted | 2024 | - |
| dc.description.edition | Universidad de Pamplona - Facultad de Ciencias Básicas. | es_CO |
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| dc.rights.accessrights | http://purl.org/coar/access_right/c_abf2 | es_CO |
| dc.type.coarversion | http://purl.org/coar/resource_type/c_2df8fbb1 | es_CO |
| Aparece en las colecciones: | Geología | |
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