Análisis morfológico de cenizas en las formaciones Las Mesas y Silencio (volcán Doña Juana Joven) e implicaciones para estudios de fragmentación
La fragmentación primaria del magma, es el mecanismo impulsor de la explosividad en erupciones volcánicas y el encargado de la producción de fragmentos piroclasticos. La determinación del estilo de fragmentación en erupciones, es una herramienta útil dentro de la gestión de riesgos para evaluar la p...
- Autores:
-
Nova Arevalo, Cristian Andrés
- Tipo de recurso:
- Trabajo de grado de pregrado
- Fecha de publicación:
- 2023
- Institución:
- Universidad de los Andes
- Repositorio:
- Séneca: repositorio Uniandes
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.uniandes.edu.co:1992/67733
- Acceso en línea:
- http://hdl.handle.net/1992/67733
- Palabra clave:
- Fragmentación primaria
Volcán Doña Juana Joven
Análisis morfotextural
Cenizas
Geociencias
- Rights
- openAccess
- License
- Attribution-NoDerivatives 4.0 Internacional
| id |
UNIANDES2_e1f060420a5d922119d739959a90e59e |
|---|---|
| oai_identifier_str |
oai:repositorio.uniandes.edu.co:1992/67733 |
| network_acronym_str |
UNIANDES2 |
| network_name_str |
Séneca: repositorio Uniandes |
| repository_id_str |
|
| dc.title.none.fl_str_mv |
Análisis morfológico de cenizas en las formaciones Las Mesas y Silencio (volcán Doña Juana Joven) e implicaciones para estudios de fragmentación |
| title |
Análisis morfológico de cenizas en las formaciones Las Mesas y Silencio (volcán Doña Juana Joven) e implicaciones para estudios de fragmentación |
| spellingShingle |
Análisis morfológico de cenizas en las formaciones Las Mesas y Silencio (volcán Doña Juana Joven) e implicaciones para estudios de fragmentación Fragmentación primaria Volcán Doña Juana Joven Análisis morfotextural Cenizas Geociencias |
| title_short |
Análisis morfológico de cenizas en las formaciones Las Mesas y Silencio (volcán Doña Juana Joven) e implicaciones para estudios de fragmentación |
| title_full |
Análisis morfológico de cenizas en las formaciones Las Mesas y Silencio (volcán Doña Juana Joven) e implicaciones para estudios de fragmentación |
| title_fullStr |
Análisis morfológico de cenizas en las formaciones Las Mesas y Silencio (volcán Doña Juana Joven) e implicaciones para estudios de fragmentación |
| title_full_unstemmed |
Análisis morfológico de cenizas en las formaciones Las Mesas y Silencio (volcán Doña Juana Joven) e implicaciones para estudios de fragmentación |
| title_sort |
Análisis morfológico de cenizas en las formaciones Las Mesas y Silencio (volcán Doña Juana Joven) e implicaciones para estudios de fragmentación |
| dc.creator.fl_str_mv |
Nova Arevalo, Cristian Andrés |
| dc.contributor.advisor.none.fl_str_mv |
Pardo Villaveces, Natalia |
| dc.contributor.author.none.fl_str_mv |
Nova Arevalo, Cristian Andrés |
| dc.contributor.jury.none.fl_str_mv |
Sierra Rojas, Maria Isabel |
| dc.subject.keyword.none.fl_str_mv |
Fragmentación primaria Volcán Doña Juana Joven Análisis morfotextural Cenizas |
| topic |
Fragmentación primaria Volcán Doña Juana Joven Análisis morfotextural Cenizas Geociencias |
| dc.subject.themes.es_CO.fl_str_mv |
Geociencias |
| description |
La fragmentación primaria del magma, es el mecanismo impulsor de la explosividad en erupciones volcánicas y el encargado de la producción de fragmentos piroclasticos. La determinación del estilo de fragmentación en erupciones, es una herramienta útil dentro de la gestión de riesgos para evaluar la peligrosidad de los volcanes y evitar la vulnerabilidad. En este trabajo, se escogieron muestras de cenizas, entre finas y muy finas, para tres estaciones de las formaciones Silencio y Las Mesas, depositadas en el costado occidental del volcán Doña Juana Joven. Se generó un análisis morfotextural de componentes a diferentes escalas, con el propósito de establecer y contrastar los mecanismos de fragmentación que originaron los depósitos. En particular, se encontró para ambas erupciones, evidencia de un mecanismo de fragmentación magmática, impulsado por procesos de descompresión súbita sobre un fundido reologicamente heterogéneo. Se determinó que la gran mayoría de partículas fragmentadas se originaron a partir de material preexistente a la erupción, formando parte de un domo o de la estructura volcánica. Para el proceso de fragmentación, se asociaron repuestas frágiles del fundido a altas tasas de deformación viscoelastica ejercidas en el instante de descompresión por presencia de un magma altamente viscoso. Considerando la escasa cantidad de partículas analizadas de la Formación Las Mesas, se sugiere la elaboración de un estudio morfotextural específico centrado exclusivamente en las partículas de esta formación, con el objetivo de complementar el análisis realizado hasta el momento. |
| publishDate |
2023 |
| dc.date.accessioned.none.fl_str_mv |
2023-06-21T19:51:30Z |
| dc.date.available.none.fl_str_mv |
2023-06-21T19:51:30Z |
| dc.date.issued.none.fl_str_mv |
2023-05 |
| dc.type.es_CO.fl_str_mv |
Trabajo de grado - Pregrado |
| dc.type.driver.none.fl_str_mv |
info:eu-repo/semantics/bachelorThesis |
| dc.type.version.none.fl_str_mv |
info:eu-repo/semantics/acceptedVersion |
| dc.type.coar.none.fl_str_mv |
http://purl.org/coar/resource_type/c_7a1f |
| dc.type.content.es_CO.fl_str_mv |
Text |
| dc.type.redcol.none.fl_str_mv |
http://purl.org/redcol/resource_type/TP |
| format |
http://purl.org/coar/resource_type/c_7a1f |
| status_str |
acceptedVersion |
| dc.identifier.uri.none.fl_str_mv |
http://hdl.handle.net/1992/67733 |
| dc.identifier.instname.es_CO.fl_str_mv |
instname:Universidad de los Andes |
| dc.identifier.reponame.es_CO.fl_str_mv |
reponame:Repositorio Institucional Séneca |
| dc.identifier.repourl.es_CO.fl_str_mv |
repourl:https://repositorio.uniandes.edu.co/ |
| url |
http://hdl.handle.net/1992/67733 |
| identifier_str_mv |
instname:Universidad de los Andes reponame:Repositorio Institucional Séneca repourl:https://repositorio.uniandes.edu.co/ |
| dc.language.iso.es_CO.fl_str_mv |
spa |
| language |
spa |
| dc.relation.references.es_CO.fl_str_mv |
M Alidibirov and D. B Dingwell. Three fragmentation mechanisms for highly viscous magma under rapid decompression: Merapi volcano. Journal of volcanology and geothermal research, 100(1-4):413-421, 2000. ISSN 0377-0273. A Alvarado, L Audin, J. M Nocquet, E Jaillard, P Mothes, P Jarrín, M. Segovia, F Rolandone, and D Cisneros. Partitioning of oblique convergence in the northern andes subduction zone: Migration history and the present-day boundary of the north andean sliver in ecuador: Eastern limit of the north andean sliver. Tectonics (Washington, D.C.), 35(5):1048-1065, 2016. ISSN 0278-7407. F. Barberi, R. Cioni, M. Rosi, R. Santacroce, A. Sbrana, and R. Vecci. Magmatic and phreatomagmatic phases in explosive eruptions of vesuvius as deduced by grain-size and component analysis of the pyroclastic deposits. Journal of volcanology and geothermal research, 38(3):287-307, 1989. ISSN 0377-0273. Ralf Buttner, Pierfrancesco Dellino, and Bernd Zimanowski. Identifying magma-water interaction from the surface features of ash particles. Nature, 401(6754):688-690, 1999. R. Buttner, P. Dellino, L. La Volpe, V. Lorenz, and B. Zimanowski. Thermohydraulic explosions in phreatomagmatic eruptions as evidenced by the comparison between pyroclasts and products from molten fuel coolant interaction experiments: Thermohydraulic explosions. Journal of Geophysical Research: Solid Earth, 107(B11):ECV 5-1 ECV 5-14, 2002. ISSN 0148-0227. Ray Cas and James Wright. Volcanic successions modern and ancient: A geological approach to processes, products and successions. Springer Science & Business Media, 2012. Katharine V. Cashman and Bettina Scheu. Chapter 25 - magmatic fragmentation. In The Encyclopedia of Volcanoes, pages 459-471. Elsevier Inc, second edition edition, 2015. ISBN 0123859387. Amanda Bachtell Clarke, Tomaso Esposti Ongaro, and Alexander Belousov. Vulcanian eruptions. In The encyclopedia of volcanoes, pages 505-518. Elsevier, 2015. P Dellino, R Isaia, L La Volpe, and G Orsi. Statistical analysis of textural data from complex pyroclastic sequences: implications for fragmentation processes of the agnanomonte spina tephra (4.1 ka), phlegraean fields, southern italy. Bulletin of volcanology, 63(7):443-461, 2001. ISSN 0258-8900. C. D'Oriano, R. Cioni, A. Bertagnini, D. Andronico, and P. D. Cole. Dynamics of ashdominated eruptions at vesuvius: the post-512 ad as1a event. Bulletin of volcanology, 73(6):699-715, 2011. ISSN 0258-8900. Orkun Ersoy, Gary Chinga, Erkan Aydar, Alain Gourgaud, H. Evren Cubukcu, and Inan Ulusoy. Texture discrimination of volcanic ashes from different fragmentation mechanisms: A case study, mount nemrut stratovolcano, eastern turkey. Computers geosciences, 32(7):936-946, 2006. ISSN 0098-3004. Richard V Fisher, Hans-Ulrich Schmincke, and Hans-Ulrich Schmincke. Pyroclastic fragments and deposits. Pyroclastic rocks, pages 89-124, 1984. Helge M Gonnermann. Magma fragmentation. Annual review of earth and planetary sciences, 43(1):431-458, 2015. ISSN 0084-6597. L. Gurioli, D. Andronico, P. Bachelery, H. Balcone-Boissard, J. Battaglia, G. Boudon, A. Burgisser, M. R. Burton, K. Cashman, S. Cichy, R. Cioni, A. Di Muro, L. Dominguez, C. D'Oriano, T. Druitt, A. J. L. Harris, M. Hort, K. Kelfoun, J. C. Komorowski, U. Kueppers, J. L. Le Pennec, T. Menand, R. Paris, L. Pioli, M. Pistolesi, M. Polacci, M. Pompilio, M. Ripepe, O. Roche, E. Rose-Koga, A. Rust, F. Schiavi, L. Scharff, R. Sulpizio, J. Taddeucci, and T. Thordarson. Memovolc consensual document: a review of cross-disciplinary approaches to characterizing small explosive magmatic eruptions. Bulletin of volcanology, 77(6):1-33, 2015. ISSN 0258-8900. M L Hall and C A Wood. Volcano-tectonic segmentation of the northern andes. Geology (Boulder), 13(3):203-207, 1985. ISSN 0091-7613. Grant Heiken. Morphology and petrography of volcanic ashes. Geological Society of America bulletin, 83(7):1961-1987, 1972. ISSN 0016-7606. Thomas J. Jones, Katharine V. Cashman, Emma J. Liu, Alison C. Rust, and Bettina Scheu. Magma fragmentation: a perspective on emerging topics and future directions. Bulletin of volcanology, 84(5), 2022. ISSN 1432-0819. E. J. Liu, K. V. Cashman, A. C. Rust, and A. H¨oskuldsson. Contrasting mechanisms of magma fragmentation during coeval magmatic and hydromagmatic activity: the hverfjall fires fissure eruption, iceland. Bulletin of volcanology, 79(10):1, 2017. ISSN 0258-8900. Keiko Matsumoto and Nobuo Geshi. Shallow crystallization of eruptive magma inferred from volcanic ash microtextures: a case study of the 2018 eruption of shinmoedake volcano, japan. Bulletin of volcanology, 83(5), 2021. ISSN 0258-8900. ML Monsalve-Bustamante. The volcanic front in colombia: Segmentation and recent and historical activity. page 97-159, 2020. J-M. Nocquet, J. C. Villegas-Lanza, M. Chlieh, P. A. Mothes, F. Rolandone, P. Jarrin, D. Cisneros, A. Alvarado, L. Audin, F. Bondoux, X. Martin, Y. Font, M. Regnier, M. Vallee, T. Tran, C. Beauval, J. M. Maguiña Mendoza, W. Martinez, H. Tavera, and H. Yepes. Motion of continental slivers and creeping subduction in the northern andes. Nature geoscience, 7(4):287-291, 2014. ISSN 1752-0894. D. Nurfiani and C. Bouvet de Maisonneuve. Furthering the investigation of eruption styles through quantitative shape analyses of volcanic ash particles. Journal of volcanology and geothermal research, 354:102-114, 2018. ISSN 0377-0273. Leland J. O'Driscoll, Mark A. Richards, and Eugene D. Humphreys. Nazca-south america interactions and the late eocene-late oligocene flat-slab episode in the central andes: Andean 37-25 ma flat-slab dynamics. Tectonics (Washington, D.C.), 31(2), 2012. ISSN 0278-7407. Natalia Pardo, Shane J. Cronin, K´aroly N´emeth, Marco Brenna, C. Ian Schipper, Eric Breard, James D.L. White, Jonathan Procter, Bob Stewart, Javier Agustín-Flores, Anja Moebis, Anke Zernack, G´abor Kereszturi, Gert Lube, Andreas Auer, Vince Neall, and Clel Wallace. Perils in distinguishing phreatic from phreatomagmatic ash; insights into the eruption mechanisms of the 6 august 2012 mt. tongariro eruption, new zealand. Journal of volcanology and geothermal research, 286:397-414, 2014. ISSN 0377-0273. Natalia Pardo, Bernardo Pulgarín, Valentina Betancourt, Federico Lucchi, and Luis Jeronimo Valencia. Facing geological mapping at low-latitude volcanoes: The doña juana volcanic complex study-case, sw-colombia. Journal of volcanology and geothermal research, 385:46-67, 2019. ISSN 0377-0273. Natalia Pardo, Jose D Avellaneda, Juanita Rausch, David Jaramillo-Vogel, Mariana Guti´errez, and Anneleen Foubert. Decrypting silicic magma/plug fragmentation at azufral crater lake, northern andes: insights from fine to extremely fine ash morpho-chemistry. Bulletin of Volcanology, 82:1-21, 2020. Natalia Pardo, Roberto Sulpizio, Federico Lucchi, Guido Giordano, Shane Cronin, Bernardo A Pulgarín, Matteo Roverato, Ana María Correa-Tamayo, Ricardo Camacho, and Miguel A Cabrera. Late holocene volcanic stratigraphy and eruption chronology of the dacitic young doña juana volcano, colombia. Geological Society of America bulletin, 2023. ISSN 0016-7606. James L Pindell and Lorcan Kennan. Tectonic evolution of the gulf of mexico, caribbean and northern south america in the mantle reference frame: an update. Geological Society special publication, 328(1):1-55, 2009. ISSN 0305-8719. Pierre-Simon Ross, Tobias D¨urig, Pier Paolo Comida, Nathalie Lefebvre, James D. L. White, Daniele Andronico, Simon Thivet, Julia Eychenne, and Lucia Gurioli. Standardized analysis of juvenile pyroclasts in comparative studies of primary magma fragmentation; 1. overview and workflow. Bulletin of volcanology, 84(1):13, 2022. ISSN 0258-8900. A. C. Rust and K. V. Cashman. Permeability controls on expansion and size distributions of pyroclasts: Magma expansion and fragmentation. Journal of Geophysical Research: Solid Earth, 116(B11), 2011. ISSN 0148-0227. Bettina Scheu and Donald B. Dingwell. Magma fragmentation. Reviews in mineralogy and geochemistry, 87(1):767-800, 2022. ISSN 1529-6466. S. V Sobolev and A. Y Babeyko. What drives orogeny in the andes? Geology (Boulder), 33(8):617-620, 2005. ISSN 0091-7613. Charles R Stern. Active andean volcanism: its geologic and tectonic setting. Revista geológica de Chile, 31(2):161-206, 2004. Alfredo Taboada, Luis A. Rivera, Andrés Fuenzalida, Armando Cisternas, Hervé Philip, Harmen Bijwaard, José Olaya, and Clara Rivera. Geodynamics of the northern andes: Subductions and intracontinental deformation (Colombia). Tectonics (Washington, D.C.), 19(5):787-813, 2000. ISSN 0278-7407. Shingo Takeuchi. Preeruptive magma viscosity: An important measure of magma eruptibility. Journal of Geophysical Research, 116(B10), 2011. ISSN 0148-0227. Yoshiyuki Tatsumi. Formation of the volcanic front in subduction zones. Geophysical research letters, 13(8):717-720, 1986. ISSN 0094-8276. Jozua van Otterloo, Ray A.F. Cas, and Ceinwen R. Scutter. The fracture behaviour of volcanic glass and relevance to quench fragmentation during formation of hyaloclastite and phreatomagmatism. Earth-science reviews, 151:79-116, 2015. ISSN 0012-8252. James D. L White and Greg A Valentine. Magmatic versus phreatomagmatic fragmentation; absence of evidence is not evidence of absence. Geosphere (Boulder, Colo.), 12 (5):1478-1488, 2016. ISSN 1553-040X. JDL White and BF Houghton. Primary volcaniclastic rocks. Geology, 34(8):677-680, 2006. K. Wohletz and Michael Sheridan. Hydrovolcanic explosions ii evolution of basaltic tuff rings and tuff cones. American Journal of Science, 283, 05 1983. doi: 10.2475/ajs.283. 5.385. Kenneth H. Wohletz. Mechanisms of hydrovolcanic pyroclast formation: Grain-size, scanning electron microscopy, and experimental studies. Journal of volcanology and geothermal research, 17(1):31-63, 1983. ISSN 0377-0273. Kenneth H Wohletz. Chemical and textural surface features of pyroclasts from hydrovolcanic eruption sequences. Technical report, Los Alamos National Lab.(US), 1987. Bernd Zimanowski, Kenneth Wohletz, Pierfrancesco Dellino, and Ralf Buttner. The volcanic ash problem. Journal of volcanology and geothermal research, 122(1):1-5, 2003. ISSN 0377-0273. Bernd Zimanowski, Ralf B¨uttner, Pierfrancesco Dellino, James D.L. White, and Kenneth H. Wohletz. Chapter 26 - magma-water interaction and phreatomagmatic fragmentation. In The Encyclopedia of Volcanoes, pages 473-484. Elsevier Inc, second edition edition, 2015. ISBN 9780123859396. |
| dc.rights.license.spa.fl_str_mv |
Attribution-NoDerivatives 4.0 Internacional |
| dc.rights.uri.*.fl_str_mv |
http://creativecommons.org/licenses/by-nd/4.0/ |
| dc.rights.accessrights.spa.fl_str_mv |
info:eu-repo/semantics/openAccess |
| dc.rights.coar.spa.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
| rights_invalid_str_mv |
Attribution-NoDerivatives 4.0 Internacional http://creativecommons.org/licenses/by-nd/4.0/ http://purl.org/coar/access_right/c_abf2 |
| eu_rights_str_mv |
openAccess |
| dc.format.extent.es_CO.fl_str_mv |
36 páginas |
| dc.format.mimetype.es_CO.fl_str_mv |
application/pdf |
| dc.publisher.es_CO.fl_str_mv |
Universidad de los Andes |
| dc.publisher.program.es_CO.fl_str_mv |
Geociencias |
| dc.publisher.faculty.es_CO.fl_str_mv |
Facultad de Ciencias |
| dc.publisher.department.es_CO.fl_str_mv |
Departamento de Geociencias |
| institution |
Universidad de los Andes |
| bitstream.url.fl_str_mv |
https://repositorio.uniandes.edu.co/bitstreams/44082328-35fb-4b96-81da-87ae33ca865d/download https://repositorio.uniandes.edu.co/bitstreams/af6af7b4-b2e7-41fe-839d-30ff574bd6f9/download https://repositorio.uniandes.edu.co/bitstreams/a8ff0417-ef85-497b-a4b6-d29fe2b3182a/download https://repositorio.uniandes.edu.co/bitstreams/54098a90-7d66-4344-9f91-4af1a850a2e0/download https://repositorio.uniandes.edu.co/bitstreams/f135950e-569a-4e19-a613-38051f014a5b/download https://repositorio.uniandes.edu.co/bitstreams/d1930bc0-2162-4be6-9d9d-145d62531ce6/download https://repositorio.uniandes.edu.co/bitstreams/f80c2d08-adab-4ce0-8061-12a5380ef2ff/download https://repositorio.uniandes.edu.co/bitstreams/a97db655-3d80-4b47-a9b4-549feeb77866/download |
| bitstream.checksum.fl_str_mv |
28f07b4fa157f063d615e6148dbaff97 7744bd7602c6cc6dcaaba35a1cf322d2 f7d494f61e544413a13e6ba1da2089cd 5aa5c691a1ffe97abd12c2966efcb8d6 97f6be4f0f0891086caaad5e5164ae35 08b106dfeb12472e88207a069e15ba30 c31f764feb7725ecc4307ddd421c04be 03b53f0e493197f117789ec1dca74046 |
| bitstream.checksumAlgorithm.fl_str_mv |
MD5 MD5 MD5 MD5 MD5 MD5 MD5 MD5 |
| repository.name.fl_str_mv |
Repositorio institucional Séneca |
| repository.mail.fl_str_mv |
adminrepositorio@uniandes.edu.co |
| _version_ |
1812134048372359168 |
| spelling |
Attribution-NoDerivatives 4.0 Internacionalhttp://creativecommons.org/licenses/by-nd/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Pardo Villaveces, Nataliavirtual::15642-1Nova Arevalo, Cristian Andrés103c1f3f-2b60-4d9d-8fee-696deb0a273d600Sierra Rojas, Maria Isabel2023-06-21T19:51:30Z2023-06-21T19:51:30Z2023-05http://hdl.handle.net/1992/67733instname:Universidad de los Andesreponame:Repositorio Institucional Sénecarepourl:https://repositorio.uniandes.edu.co/La fragmentación primaria del magma, es el mecanismo impulsor de la explosividad en erupciones volcánicas y el encargado de la producción de fragmentos piroclasticos. La determinación del estilo de fragmentación en erupciones, es una herramienta útil dentro de la gestión de riesgos para evaluar la peligrosidad de los volcanes y evitar la vulnerabilidad. En este trabajo, se escogieron muestras de cenizas, entre finas y muy finas, para tres estaciones de las formaciones Silencio y Las Mesas, depositadas en el costado occidental del volcán Doña Juana Joven. Se generó un análisis morfotextural de componentes a diferentes escalas, con el propósito de establecer y contrastar los mecanismos de fragmentación que originaron los depósitos. En particular, se encontró para ambas erupciones, evidencia de un mecanismo de fragmentación magmática, impulsado por procesos de descompresión súbita sobre un fundido reologicamente heterogéneo. Se determinó que la gran mayoría de partículas fragmentadas se originaron a partir de material preexistente a la erupción, formando parte de un domo o de la estructura volcánica. Para el proceso de fragmentación, se asociaron repuestas frágiles del fundido a altas tasas de deformación viscoelastica ejercidas en el instante de descompresión por presencia de un magma altamente viscoso. Considerando la escasa cantidad de partículas analizadas de la Formación Las Mesas, se sugiere la elaboración de un estudio morfotextural específico centrado exclusivamente en las partículas de esta formación, con el objetivo de complementar el análisis realizado hasta el momento.Primary magma fragmentation is the driving mechanism of explosivity in volcanic eruptions and is responsible for the production of pyroclastic fragments. The determination of the fragmentation style in eruptions is a useful tool in risk management to evaluate the danger of volcanoes and to avoid vulnerability. In this work, samples of fine to very fine ashes were selected for three stations of the Silencio and Las Mesas formations, deposited on the western side of the Doña Juana Joven volcano. A morpho-textural analysis of components at different scales was generated, with the purpose of establishing and contrasting the fragmentation mechanisms that originated the deposits. In particular, evidence of a magmatic fragmentation mechanism, driven by sudden decompression processes on a rheologically heterogeneous melt, was found for both eruptions. It was determined that the vast majority of fragmented particles originated from material that pre-existed the eruption, forming part of a dome or volcanic structure. For the fragmentation process, fragile melt responses were associated with high rates of viscoelastic deformation exerted at the instant of decompression due to the presence of a highly viscous magma. Considering the small amount of analyzed particles from the Las Mesas Formation, we suggest the elaboration of a specific morphotectural study focused exclusively on the particles of this formation, in order to complement the analysis carried out so far.GeocientíficoPregradoVulcanología36 páginasapplication/pdfspaUniversidad de los AndesGeocienciasFacultad de CienciasDepartamento de GeocienciasAnálisis morfológico de cenizas en las formaciones Las Mesas y Silencio (volcán Doña Juana Joven) e implicaciones para estudios de fragmentaciónTrabajo de grado - Pregradoinfo:eu-repo/semantics/bachelorThesisinfo:eu-repo/semantics/acceptedVersionhttp://purl.org/coar/resource_type/c_7a1fTexthttp://purl.org/redcol/resource_type/TPFragmentación primariaVolcán Doña Juana JovenAnálisis morfotexturalCenizasGeocienciasM Alidibirov and D. B Dingwell. Three fragmentation mechanisms for highly viscous magma under rapid decompression: Merapi volcano. Journal of volcanology and geothermal research, 100(1-4):413-421, 2000. ISSN 0377-0273.A Alvarado, L Audin, J. M Nocquet, E Jaillard, P Mothes, P Jarrín, M. Segovia, F Rolandone, and D Cisneros. Partitioning of oblique convergence in the northern andes subduction zone: Migration history and the present-day boundary of the north andean sliver in ecuador: Eastern limit of the north andean sliver. Tectonics (Washington, D.C.), 35(5):1048-1065, 2016. ISSN 0278-7407.F. Barberi, R. Cioni, M. Rosi, R. Santacroce, A. Sbrana, and R. Vecci. Magmatic and phreatomagmatic phases in explosive eruptions of vesuvius as deduced by grain-size and component analysis of the pyroclastic deposits. Journal of volcanology and geothermal research, 38(3):287-307, 1989. ISSN 0377-0273.Ralf Buttner, Pierfrancesco Dellino, and Bernd Zimanowski. Identifying magma-water interaction from the surface features of ash particles. Nature, 401(6754):688-690, 1999.R. Buttner, P. Dellino, L. La Volpe, V. Lorenz, and B. Zimanowski. Thermohydraulic explosions in phreatomagmatic eruptions as evidenced by the comparison between pyroclasts and products from molten fuel coolant interaction experiments: Thermohydraulic explosions. Journal of Geophysical Research: Solid Earth, 107(B11):ECV 5-1 ECV 5-14, 2002. ISSN 0148-0227.Ray Cas and James Wright. Volcanic successions modern and ancient: A geological approach to processes, products and successions. Springer Science & Business Media, 2012.Katharine V. Cashman and Bettina Scheu. Chapter 25 - magmatic fragmentation. In The Encyclopedia of Volcanoes, pages 459-471. Elsevier Inc, second edition edition, 2015. ISBN 0123859387.Amanda Bachtell Clarke, Tomaso Esposti Ongaro, and Alexander Belousov. Vulcanian eruptions. In The encyclopedia of volcanoes, pages 505-518. Elsevier, 2015.P Dellino, R Isaia, L La Volpe, and G Orsi. Statistical analysis of textural data from complex pyroclastic sequences: implications for fragmentation processes of the agnanomonte spina tephra (4.1 ka), phlegraean fields, southern italy. Bulletin of volcanology, 63(7):443-461, 2001. ISSN 0258-8900.C. D'Oriano, R. Cioni, A. Bertagnini, D. Andronico, and P. D. Cole. Dynamics of ashdominated eruptions at vesuvius: the post-512 ad as1a event. Bulletin of volcanology, 73(6):699-715, 2011. ISSN 0258-8900.Orkun Ersoy, Gary Chinga, Erkan Aydar, Alain Gourgaud, H. Evren Cubukcu, and Inan Ulusoy. Texture discrimination of volcanic ashes from different fragmentation mechanisms: A case study, mount nemrut stratovolcano, eastern turkey. Computers geosciences, 32(7):936-946, 2006. ISSN 0098-3004.Richard V Fisher, Hans-Ulrich Schmincke, and Hans-Ulrich Schmincke. Pyroclastic fragments and deposits. Pyroclastic rocks, pages 89-124, 1984.Helge M Gonnermann. Magma fragmentation. Annual review of earth and planetary sciences, 43(1):431-458, 2015. ISSN 0084-6597.L. Gurioli, D. Andronico, P. Bachelery, H. Balcone-Boissard, J. Battaglia, G. Boudon, A. Burgisser, M. R. Burton, K. Cashman, S. Cichy, R. Cioni, A. Di Muro, L. Dominguez, C. D'Oriano, T. Druitt, A. J. L. Harris, M. Hort, K. Kelfoun, J. C. Komorowski, U. Kueppers, J. L. Le Pennec, T. Menand, R. Paris, L. Pioli, M. Pistolesi, M. Polacci, M. Pompilio, M. Ripepe, O. Roche, E. Rose-Koga, A. Rust, F. Schiavi, L. Scharff, R. Sulpizio, J. Taddeucci, and T. Thordarson. Memovolc consensual document: a review of cross-disciplinary approaches to characterizing small explosive magmatic eruptions. Bulletin of volcanology, 77(6):1-33, 2015. ISSN 0258-8900.M L Hall and C A Wood. Volcano-tectonic segmentation of the northern andes. Geology (Boulder), 13(3):203-207, 1985. ISSN 0091-7613.Grant Heiken. Morphology and petrography of volcanic ashes. Geological Society of America bulletin, 83(7):1961-1987, 1972. ISSN 0016-7606.Thomas J. Jones, Katharine V. Cashman, Emma J. Liu, Alison C. Rust, and Bettina Scheu. Magma fragmentation: a perspective on emerging topics and future directions. Bulletin of volcanology, 84(5), 2022. ISSN 1432-0819.E. J. Liu, K. V. Cashman, A. C. Rust, and A. H¨oskuldsson. Contrasting mechanisms of magma fragmentation during coeval magmatic and hydromagmatic activity: the hverfjall fires fissure eruption, iceland. Bulletin of volcanology, 79(10):1, 2017. ISSN 0258-8900.Keiko Matsumoto and Nobuo Geshi. Shallow crystallization of eruptive magma inferred from volcanic ash microtextures: a case study of the 2018 eruption of shinmoedake volcano, japan. Bulletin of volcanology, 83(5), 2021. ISSN 0258-8900.ML Monsalve-Bustamante. The volcanic front in colombia: Segmentation and recent and historical activity. page 97-159, 2020.J-M. Nocquet, J. C. Villegas-Lanza, M. Chlieh, P. A. Mothes, F. Rolandone, P. Jarrin, D. Cisneros, A. Alvarado, L. Audin, F. Bondoux, X. Martin, Y. Font, M. Regnier, M. Vallee, T. Tran, C. Beauval, J. M. Maguiña Mendoza, W. Martinez, H. Tavera, and H. Yepes. Motion of continental slivers and creeping subduction in the northern andes. Nature geoscience, 7(4):287-291, 2014. ISSN 1752-0894.D. Nurfiani and C. Bouvet de Maisonneuve. Furthering the investigation of eruption styles through quantitative shape analyses of volcanic ash particles. Journal of volcanology and geothermal research, 354:102-114, 2018. ISSN 0377-0273.Leland J. O'Driscoll, Mark A. Richards, and Eugene D. Humphreys. Nazca-south america interactions and the late eocene-late oligocene flat-slab episode in the central andes: Andean 37-25 ma flat-slab dynamics. Tectonics (Washington, D.C.), 31(2), 2012. ISSN 0278-7407.Natalia Pardo, Shane J. Cronin, K´aroly N´emeth, Marco Brenna, C. Ian Schipper, Eric Breard, James D.L. White, Jonathan Procter, Bob Stewart, Javier Agustín-Flores, Anja Moebis, Anke Zernack, G´abor Kereszturi, Gert Lube, Andreas Auer, Vince Neall, and Clel Wallace. Perils in distinguishing phreatic from phreatomagmatic ash; insights into the eruption mechanisms of the 6 august 2012 mt. tongariro eruption, new zealand. Journal of volcanology and geothermal research, 286:397-414, 2014. ISSN 0377-0273.Natalia Pardo, Bernardo Pulgarín, Valentina Betancourt, Federico Lucchi, and Luis Jeronimo Valencia. Facing geological mapping at low-latitude volcanoes: The doña juana volcanic complex study-case, sw-colombia. Journal of volcanology and geothermal research, 385:46-67, 2019. ISSN 0377-0273.Natalia Pardo, Jose D Avellaneda, Juanita Rausch, David Jaramillo-Vogel, Mariana Guti´errez, and Anneleen Foubert. Decrypting silicic magma/plug fragmentation at azufral crater lake, northern andes: insights from fine to extremely fine ash morpho-chemistry. Bulletin of Volcanology, 82:1-21, 2020.Natalia Pardo, Roberto Sulpizio, Federico Lucchi, Guido Giordano, Shane Cronin, Bernardo A Pulgarín, Matteo Roverato, Ana María Correa-Tamayo, Ricardo Camacho, and Miguel A Cabrera. Late holocene volcanic stratigraphy and eruption chronology of the dacitic young doña juana volcano, colombia. Geological Society of America bulletin, 2023. ISSN 0016-7606.James L Pindell and Lorcan Kennan. Tectonic evolution of the gulf of mexico, caribbean and northern south america in the mantle reference frame: an update. Geological Society special publication, 328(1):1-55, 2009. ISSN 0305-8719.Pierre-Simon Ross, Tobias D¨urig, Pier Paolo Comida, Nathalie Lefebvre, James D. L. White, Daniele Andronico, Simon Thivet, Julia Eychenne, and Lucia Gurioli. Standardized analysis of juvenile pyroclasts in comparative studies of primary magma fragmentation; 1. overview and workflow. Bulletin of volcanology, 84(1):13, 2022. ISSN 0258-8900.A. C. Rust and K. V. Cashman. Permeability controls on expansion and size distributions of pyroclasts: Magma expansion and fragmentation. Journal of Geophysical Research: Solid Earth, 116(B11), 2011. ISSN 0148-0227.Bettina Scheu and Donald B. Dingwell. Magma fragmentation. Reviews in mineralogy and geochemistry, 87(1):767-800, 2022. ISSN 1529-6466.S. V Sobolev and A. Y Babeyko. What drives orogeny in the andes? Geology (Boulder), 33(8):617-620, 2005. ISSN 0091-7613.Charles R Stern. Active andean volcanism: its geologic and tectonic setting. Revista geológica de Chile, 31(2):161-206, 2004.Alfredo Taboada, Luis A. Rivera, Andrés Fuenzalida, Armando Cisternas, Hervé Philip, Harmen Bijwaard, José Olaya, and Clara Rivera. Geodynamics of the northern andes: Subductions and intracontinental deformation (Colombia). Tectonics (Washington, D.C.), 19(5):787-813, 2000. ISSN 0278-7407.Shingo Takeuchi. Preeruptive magma viscosity: An important measure of magma eruptibility. Journal of Geophysical Research, 116(B10), 2011. ISSN 0148-0227.Yoshiyuki Tatsumi. Formation of the volcanic front in subduction zones. Geophysical research letters, 13(8):717-720, 1986. ISSN 0094-8276.Jozua van Otterloo, Ray A.F. Cas, and Ceinwen R. Scutter. The fracture behaviour of volcanic glass and relevance to quench fragmentation during formation of hyaloclastite and phreatomagmatism. Earth-science reviews, 151:79-116, 2015. ISSN 0012-8252.James D. L White and Greg A Valentine. Magmatic versus phreatomagmatic fragmentation; absence of evidence is not evidence of absence. Geosphere (Boulder, Colo.), 12 (5):1478-1488, 2016. ISSN 1553-040X.JDL White and BF Houghton. Primary volcaniclastic rocks. Geology, 34(8):677-680, 2006.K. Wohletz and Michael Sheridan. Hydrovolcanic explosions ii evolution of basaltic tuff rings and tuff cones. American Journal of Science, 283, 05 1983. doi: 10.2475/ajs.283. 5.385.Kenneth H. Wohletz. Mechanisms of hydrovolcanic pyroclast formation: Grain-size, scanning electron microscopy, and experimental studies. Journal of volcanology and geothermal research, 17(1):31-63, 1983. ISSN 0377-0273.Kenneth H Wohletz. Chemical and textural surface features of pyroclasts from hydrovolcanic eruption sequences. Technical report, Los Alamos National Lab.(US), 1987.Bernd Zimanowski, Kenneth Wohletz, Pierfrancesco Dellino, and Ralf Buttner. The volcanic ash problem. Journal of volcanology and geothermal research, 122(1):1-5, 2003. ISSN 0377-0273.Bernd Zimanowski, Ralf B¨uttner, Pierfrancesco Dellino, James D.L. White, and Kenneth H. Wohletz. Chapter 26 - magma-water interaction and phreatomagmatic fragmentation. In The Encyclopedia of Volcanoes, pages 473-484. Elsevier Inc, second edition edition, 2015. ISBN 9780123859396.201913525Publicationhttps://scholar.google.es/citations?user=ikmh8i0AAAAJvirtual::15642-10000-0002-8247-4116virtual::15642-1https://scienti.minciencias.gov.co/cvlac/visualizador/generarCurriculoCv.do?cod_rh=0000406740virtual::15642-1a782b64a-d94d-4fd1-b866-03e18a0b504fvirtual::15642-1a782b64a-d94d-4fd1-b866-03e18a0b504fvirtual::15642-1THUMBNAILAnálisis morfológico de cenizas en las formaciones Las Mesas y Silencio volcán Doña Juana Joven e implicaciones para estudios de fragmentación.pdf.jpgAnálisis morfológico de cenizas en las formaciones Las Mesas y Silencio volcán Doña Juana Joven e implicaciones para estudios de fragmentación.pdf.jpgIM Thumbnailimage/jpeg8998https://repositorio.uniandes.edu.co/bitstreams/44082328-35fb-4b96-81da-87ae33ca865d/download28f07b4fa157f063d615e6148dbaff97MD56Formato autorizacion tesis.pdf.jpgFormato autorizacion tesis.pdf.jpgIM Thumbnailimage/jpeg15930https://repositorio.uniandes.edu.co/bitstreams/af6af7b4-b2e7-41fe-839d-30ff574bd6f9/download7744bd7602c6cc6dcaaba35a1cf322d2MD58CC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; charset=utf-8799https://repositorio.uniandes.edu.co/bitstreams/a8ff0417-ef85-497b-a4b6-d29fe2b3182a/downloadf7d494f61e544413a13e6ba1da2089cdMD52LICENSElicense.txtlicense.txttext/plain; charset=utf-81810https://repositorio.uniandes.edu.co/bitstreams/54098a90-7d66-4344-9f91-4af1a850a2e0/download5aa5c691a1ffe97abd12c2966efcb8d6MD51TEXTAnálisis morfológico de cenizas en las formaciones Las Mesas y Silencio volcán Doña Juana Joven e implicaciones para estudios de fragmentación.pdf.txtAnálisis morfológico de cenizas en las formaciones Las Mesas y Silencio volcán Doña Juana Joven e implicaciones para estudios de fragmentación.pdf.txtExtracted texttext/plain73569https://repositorio.uniandes.edu.co/bitstreams/f135950e-569a-4e19-a613-38051f014a5b/download97f6be4f0f0891086caaad5e5164ae35MD55Formato autorizacion tesis.pdf.txtFormato autorizacion tesis.pdf.txtExtracted texttext/plain1161https://repositorio.uniandes.edu.co/bitstreams/d1930bc0-2162-4be6-9d9d-145d62531ce6/download08b106dfeb12472e88207a069e15ba30MD57ORIGINALAnálisis morfológico de cenizas en las formaciones Las Mesas y Silencio volcán Doña Juana Joven e implicaciones para estudios de fragmentación.pdfAnálisis morfológico de cenizas en las formaciones Las Mesas y Silencio volcán Doña Juana Joven e implicaciones para estudios de fragmentación.pdfTrabajo de gradoapplication/pdf21129865https://repositorio.uniandes.edu.co/bitstreams/f80c2d08-adab-4ce0-8061-12a5380ef2ff/downloadc31f764feb7725ecc4307ddd421c04beMD53Formato autorizacion tesis.pdfFormato autorizacion tesis.pdfHIDEapplication/pdf274057https://repositorio.uniandes.edu.co/bitstreams/a97db655-3d80-4b47-a9b4-549feeb77866/download03b53f0e493197f117789ec1dca74046MD541992/67733oai:repositorio.uniandes.edu.co:1992/677332024-03-13 15:30:57.937http://creativecommons.org/licenses/by-nd/4.0/open.accesshttps://repositorio.uniandes.edu.coRepositorio institucional Sénecaadminrepositorio@uniandes.edu.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 |