Análisis de componentes en tefras de corrientes piroclásticas de la Fm. El Silencio, Complejo Volcánico Doña Juana, Nariño
Las erupciones vulcanianas son uno de los eventos naturales más destructivos, es por eso por lo que el estudio y análisis de sus erupciones y sus registros es sumamente importante para la prevención de riesgos. En el presente proyecto se estudiarán depósitos de corrientes piroclásticas correspondien...
- Autores:
-
Enciso Hernández, Nicolás
- Tipo de recurso:
- Trabajo de grado de pregrado
- Fecha de publicación:
- 2020
- Institución:
- Universidad de los Andes
- Repositorio:
- Séneca: repositorio Uniandes
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.uniandes.edu.co:1992/59761
- Acceso en línea:
- http://hdl.handle.net/1992/59761
- Palabra clave:
- Doña Juana Joven
Corrientes piroclásticas
Mecanismos de transporte
Granulometría
Texturas de desequilibrio
Análisis de componentes
Geociencias
- Rights
- openAccess
- License
- Atribución 4.0 Internacional
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Análisis de componentes en tefras de corrientes piroclásticas de la Fm. El Silencio, Complejo Volcánico Doña Juana, Nariño |
| title |
Análisis de componentes en tefras de corrientes piroclásticas de la Fm. El Silencio, Complejo Volcánico Doña Juana, Nariño |
| spellingShingle |
Análisis de componentes en tefras de corrientes piroclásticas de la Fm. El Silencio, Complejo Volcánico Doña Juana, Nariño Doña Juana Joven Corrientes piroclásticas Mecanismos de transporte Granulometría Texturas de desequilibrio Análisis de componentes Geociencias |
| title_short |
Análisis de componentes en tefras de corrientes piroclásticas de la Fm. El Silencio, Complejo Volcánico Doña Juana, Nariño |
| title_full |
Análisis de componentes en tefras de corrientes piroclásticas de la Fm. El Silencio, Complejo Volcánico Doña Juana, Nariño |
| title_fullStr |
Análisis de componentes en tefras de corrientes piroclásticas de la Fm. El Silencio, Complejo Volcánico Doña Juana, Nariño |
| title_full_unstemmed |
Análisis de componentes en tefras de corrientes piroclásticas de la Fm. El Silencio, Complejo Volcánico Doña Juana, Nariño |
| title_sort |
Análisis de componentes en tefras de corrientes piroclásticas de la Fm. El Silencio, Complejo Volcánico Doña Juana, Nariño |
| dc.creator.fl_str_mv |
Enciso Hernández, Nicolás |
| dc.contributor.advisor.none.fl_str_mv |
Pardo Villaveces, Natalia |
| dc.contributor.author.none.fl_str_mv |
Enciso Hernández, Nicolás |
| dc.contributor.jury.none.fl_str_mv |
Eickmann, Benjamin |
| dc.subject.keyword.none.fl_str_mv |
Doña Juana Joven Corrientes piroclásticas Mecanismos de transporte Granulometría Texturas de desequilibrio Análisis de componentes |
| topic |
Doña Juana Joven Corrientes piroclásticas Mecanismos de transporte Granulometría Texturas de desequilibrio Análisis de componentes Geociencias |
| dc.subject.themes.es_CO.fl_str_mv |
Geociencias |
| description |
Las erupciones vulcanianas son uno de los eventos naturales más destructivos, es por eso por lo que el estudio y análisis de sus erupciones y sus registros es sumamente importante para la prevención de riesgos. En el presente proyecto se estudiarán depósitos de corrientes piroclásticas correspondientes al Complejo Volcánico de Doña Juana, Nariño. Para el desarrollo de este proyecto se eligieron tres muestras ubicadas en tres distancias distintas del Doña Juana Joven. Sobre dichas muestras se realizó un análisis granulométrico para elegir las tres subpoblaciones más significativas de cada muestra. El conteo con la lupa binocular de cenizas gruesas arrojó una mayor proporción de líticos respecto a los demás componentes; el conteo de las poblaciones más finas con microscopio óptico permitió identificar los posibles líticos juveniles rojos y gris. Los resultados obtenidos permiten estudiar el control topográfico y el efecto de la segregación de densidad en el transporte de corrientes piroclásticas. |
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2020 |
| dc.date.issued.none.fl_str_mv |
2020 |
| dc.date.accessioned.none.fl_str_mv |
2022-08-10T13:29:51Z |
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2022-08-10T13:29:51Z |
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Trabajo de grado - Pregrado |
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info:eu-repo/semantics/bachelorThesis |
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Petrology, geochemistry, and correlation of tephra deposits from a large early-holocene eruption of Mentolat Volcano, Southern Chile. Journal of South American Earth Sciences, 90, 282¿ 295. https://doi.org/10.1016/j.jsames.2018.12.020 Wohletz, K. H., Sheridan, M. F., & Brown, W. K. (1989). Particle size distributions and the sequential fragmentation/transport theory applied to volcanic ash. Journal of Geophysical Research: Solid Earth, 94(B11), 15703¿15721. https://doi.org/10.1029/jb094ib11p15703 |
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Atribución 4.0 Internacionalhttp://creativecommons.org/licenses/by-nc-sa/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Pardo Villaveces, Nataliacfd09924-52fd-4cb1-a995-09f18aff0fc9600Enciso Hernández, Nicolásff00f038-ad9a-4f63-8570-9d7130ea7b06600Eickmann, Benjamin2022-08-10T13:29:51Z2022-08-10T13:29:51Z2020http://hdl.handle.net/1992/59761instname:Universidad de los Andesreponame:Repositorio Institucional Sénecarepourl:https://repositorio.uniandes.edu.co/Las erupciones vulcanianas son uno de los eventos naturales más destructivos, es por eso por lo que el estudio y análisis de sus erupciones y sus registros es sumamente importante para la prevención de riesgos. En el presente proyecto se estudiarán depósitos de corrientes piroclásticas correspondientes al Complejo Volcánico de Doña Juana, Nariño. Para el desarrollo de este proyecto se eligieron tres muestras ubicadas en tres distancias distintas del Doña Juana Joven. Sobre dichas muestras se realizó un análisis granulométrico para elegir las tres subpoblaciones más significativas de cada muestra. El conteo con la lupa binocular de cenizas gruesas arrojó una mayor proporción de líticos respecto a los demás componentes; el conteo de las poblaciones más finas con microscopio óptico permitió identificar los posibles líticos juveniles rojos y gris. Los resultados obtenidos permiten estudiar el control topográfico y el efecto de la segregación de densidad en el transporte de corrientes piroclásticas.GeocientíficoPregradoVulcanología41 paginasapplication/pdfspaUniversidad de los AndesGeocienciasFacultad de CienciasDepartamento de GeocienciasAnálisis de componentes en tefras de corrientes piroclásticas de la Fm. El Silencio, Complejo Volcánico Doña Juana, NariñoTrabajo de grado - Pregradoinfo:eu-repo/semantics/bachelorThesisinfo:eu-repo/semantics/acceptedVersionhttp://purl.org/coar/resource_type/c_7a1fTexthttp://purl.org/redcol/resource_type/TPDoña Juana JovenCorrientes piroclásticasMecanismos de transporteGranulometríaTexturas de desequilibrioAnálisis de componentesGeocienciasAngkasa, S. S., Ohba, T., Imura, T., Setiawan, I., & Rosana, M. (2019). Tephra-stratigraphy and Ash Componentry Studies of proximal volcanic products at Mount Tangkuban Parahu, Indonesia: An insight to holocene volcanic activity. Indonesian Journal on Geoscience, 6(3). https://doi.org/10.17014/ijog.6.3.235-253Benet, D., Costa, F., Pedreros, G., & Cardona, C. (2021). The volcanic ash record of shallow magma intrusion and dome emplacement at Nevados de Chillán volcanic complex, Chile. Journal of Volcanology and Geothermal Research, 417, 107308. https://doi.org/10.1016/j.jvolgeores.2021.107308Benjamin J. Andrews, Michael Manga; Effects of topography on pyroclastic density current runout and formation of coignimbrites. Geology 2011;; 39 (12): 1099¿1102. doi: https://doi.org/10.1130/G32226.1Buckley, V.J.E., Sparks, R.S.J. & Wood, B.J. Hornblende dehydration reactions during magma ascent at Soufrière Hills Volcano, Montserrat. Contrib Mineral Petrol 151, 121¿140 (2006). https://doi.org/10.1007/s00410-005-0060-5Bustillos A., J. E., Romero, J. E., Guevara C., A., & Díaz-Alvarado, J. (2017). Tephra fallout from the long-lasting tungurahua eruptive cycle (1999-2014): Variations through eruptive style transition and deposition processes. Andean Geology, 45(1), 47. https://doi.org/10.5027/andgeov45n1-3036Branney, M. J., Kokelaar, P., & Kokelaar, B. P. (2002). Pyroclastic density currents and the sedimentation of ignimbrites. Geological Society of LondonBlott, S. J., & Pye, K. (2001). GRADISTAT: a grain size distribution and statistics package for the analysis of unconsolidated sediments. Earth surface processes and Landforms, 26(11), 1237-1248.Cas, R. A. F., & Wright, J. V. (1988). Volcanic successions modern and ancient: A geological approach to processes, products and successions (Vol. 2). Chapman and Hall.Cashman, K. V., & Scheu, B. (2015). Magmatic fragmentation. In The encyclopedia of volcanoes (pp. 459-471). Academic Press.Cediel, F., Shaw, R. P., & Cáceres, C. (2003). Tectonic assembly of the northern Andean blockCioni, R., Bertagnini, A., Andronico, D., Cole, P. D., & Mundula, F. (2011). The 512 AD eruption of vesuvius: Complex dynamics of a small scale Subplinian event. Bulletin of Volcanology, 73(7), 789¿810. https://doi.org/10.1007/s00445-011-0454-3Comida PP, Ross P-S, Dürig T, White JDL, Lefebvre N (2021) Standardized analysis of juvenile pyroclasts in comparative studies of primary magma fragmentation; 2. Choice of size fractions and method optimization. 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Bull Volcanol 75: doi:10.1007/s00445-013-0695-4Lücke, O. H., & Calderón, A. (2016). Characterization of the ashes from the 2014-2015 turrialba volcano eruptions by means of scanning electron microscopy and energy dispersive X-ray spectroscopy. Revista Geológica De América Central, 54. https://doi.org/10.15517/rgac.v54i0.23281Martinez, D. (2020). Análisis de distribución de tamaños de partículas aplicados a corrientes piroclásticas del Holoceno en el Volcán Doña Juana, Nariño. [Tesis de pregrado, Universidad de los Andes].Marino, E., González, F. J., Kuhn, T., Madureira, P., Wegorzewski, A. V., Mirao, J., Medialdea, T., Oeser, M., Miguel, C., Reyes, J., Somoza, L., & Lunar, R. (2019). Hydrogenetic, Diagenetic and Hydrothermal Processes Forming Ferromanganese Crusts in the Canary IslandMatsumoto, K., Geshi, N. Shallow crystallization of eruptive magma inferred from volcanic ash microtextures: a case study of the 2018 eruption of Shinmoedake volcano, Japan. 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Journal of Geophysical Research: Solid Earth, 94(B11), 15703¿15721. https://doi.org/10.1029/jb094ib11p1570320151454PublicationORIGINALTesis biblioteca.pdfTesis biblioteca.pdfTrabajo de grado en PDFapplication/pdf3534586https://repositorio.uniandes.edu.co/bitstreams/ad532650-e1a3-42e0-badb-43c685d23e93/downloaddf0cd884d61e426dc7b21c79abfe625cMD53Anexos.pdfAnexos.pdfAnexos de conteosapplication/pdf471520https://repositorio.uniandes.edu.co/bitstreams/b996c71e-a782-4c92-ad69-4b7b8921c514/downloadd28a38f965342215087e621b5e31333aMD59Formatos de autorización final.pdfFormatos de autorización final.pdfHIDEapplication/pdf512261https://repositorio.uniandes.edu.co/bitstreams/46b665bf-b13b-4802-be1c-dd84058aa841/download902eebdea980c5cd2dcc7fd3ad443ca8MD510CC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; charset=utf-8908https://repositorio.uniandes.edu.co/bitstreams/53c80ec9-87df-4090-a276-3d30f9e48028/download0175ea4a2d4caec4bbcc37e300941108MD58THUMBNAILTesis biblioteca.pdf.jpgTesis biblioteca.pdf.jpgIM Thumbnailimage/jpeg5923https://repositorio.uniandes.edu.co/bitstreams/a5d98214-1f6c-427d-bbad-0b0eb0aa44e0/downloadec5c7c30c0e44762c27e6ab3ce89097bMD512Anexos.pdf.jpgAnexos.pdf.jpgIM Thumbnailimage/jpeg11031https://repositorio.uniandes.edu.co/bitstreams/db8d5775-23a1-4597-a8d1-9575855eb8ea/downloadfaffb7be038e81b1cdef5f2c9b2c1ad0MD514Formatos de autorización final.pdf.jpgFormatos de autorización final.pdf.jpgIM Thumbnailimage/jpeg15734https://repositorio.uniandes.edu.co/bitstreams/495ed328-ca47-45eb-b71c-be2ca611538c/download9bbf427668565360c367633e38d37224MD516TEXTTesis biblioteca.pdf.txtTesis biblioteca.pdf.txtExtracted texttext/plain61836https://repositorio.uniandes.edu.co/bitstreams/34224c31-ccbf-4191-bf48-af86694a12b6/download0816943a3c529ce0c02f6cd42fbe975cMD511Anexos.pdf.txtAnexos.pdf.txtExtracted texttext/plain3605https://repositorio.uniandes.edu.co/bitstreams/00afc4b0-08ba-4b54-be5b-ef909d1e4080/downloaddfa946d55bd57ef99686ef96dbc0c19dMD513Formatos de autorización final.pdf.txtFormatos de autorización final.pdf.txtExtracted texttext/plain1389https://repositorio.uniandes.edu.co/bitstreams/37060635-b959-4221-b36c-fd7c4e31ab28/download367178a62dcef01fa69a9f311b1bcbbcMD515LICENSElicense.txtlicense.txttext/plain; charset=utf-81810https://repositorio.uniandes.edu.co/bitstreams/883cb5d5-8467-454a-b17e-3899b2854301/download5aa5c691a1ffe97abd12c2966efcb8d6MD571992/59761oai:repositorio.uniandes.edu.co:1992/597612024-03-20 11:46:21.844http://creativecommons.org/licenses/by-nc-sa/4.0/restrictedhttps://repositorio.uniandes.edu.coRepositorio institucional Sénecaadminrepositorio@uniandes.edu.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 |