dor_id: 4132296

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510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

561.#.#.u: https://www.geofisica.unam.mx/

650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

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270.#.#.d: MX

270.1.#.d: México

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883.#.#.a: Revistas UNAM

590.#.#.a: Coordinación de Difusión Cultural

883.#.#.1: https://www.publicaciones.unam.mx/

883.#.#.q: Dirección General de Publicaciones y Fomento Editorial

850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/334/325

100.1.#.a: Rouwet, D.; Bellomo, S.; Brusca, L.; Inguaggiato, S.; Jutzeler, M.; Mora, R.; Mazot, A.; Bernard, R.; Cassidy, M.; Taran, Y.

524.#.#.a: Rouwet, D., et al. (2009). Major and trace element geochemistry of El Chichón volcano-hydrothermal system (Chiapas, México) in. Geofísica Internacional; Vol. 48 Núm. 1: Enero 1, 2009; 55-72. Recuperado de https://repositorio.unam.mx/contenidos/4132296

245.1.0.a: Major and trace element geochemistry of El Chichón volcano-hydrothermal system (Chiapas, México) in

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2009

264.#.1.c: 2009-01-01

653.#.#.a: El Chichón; geoquímica de fluidos; monitoreo volcánico; El Chichón; fluid geochemistry; volcanic surveillance

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/334

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/334

041.#.7.h: spa

520.3.#.a: Isotopic, major and trace element composition studies for the crater lake, the Soap Pool and thermal springs at El Chichón volcano in November 2006-October 2007 confirm the complex relationship between annual rainfall distribution and crater lake volume and chemistry. In 2001, 2004 and 2007 high volume high-Cl lake may be related to reactivation of high discharge (>10 kg/s) saline near-neutral water from the Soap Pool boiling springs into the lake, a few months (~January) after the end of the rainy season (June-October). The peak lake volume occurred in March 2007 (~6 x 105 m3). Agua Tibia 2 thermal springs discharge near the foot of the SW dome but their chemistry suggests a lower temperature regime, an enhanced water-rock interaction and basement contribution (evaporites and carbonates), anhydrite leaching from the 1982 pyroclastic deposits, rather than dome activity. New suggestions of crater lake seepage are evidenced by the Agua Caliente thermal springs. Existing models on the “crater lake-Soap Pool spring” and the deep hydrothermal system are discussed. Chemical changes in the deep geothermal aquifer feeding the thermal springs may predict dome rise. Future volcanic surveillance should focus on spring chemistry variations, as well as crater lake monitoring.doi: https://doi.org/10.22201/igeof.00167169p.2009.48.1.99

773.1.#.t: Geofísica Internacional; Vol. 48 Núm. 1: Enero 1, 2009; 55-72

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

310.#.#.a: Trimestral

300.#.#.a: Páginas: 55-72

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.00167169p.2009.48.1.99

handle: 68b7852c93f15262

harvesting_date: 2023-06-20 16:00:00.0

856.#.0.q: application/pdf

file_creation_date: 2009-01-21 15:44:15.0

file_modification_date: 2022-05-30 14:16:03.0

file_creator: Rouwet D.

file_name: a3c53946a8103a061ddafd45f3002f5575c581418eea87e58919631841ba822e.pdf

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245.1.0.b: Major and trace element geochemistry of El Chichón volcano-hydrothermal system (Chiapas, México) in 2006-2007: implications for future geochemical monitoring

last_modified: 2023-06-20 16:00:00

license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es

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Artículo

Major and trace element geochemistry of El Chichón volcano-hydrothermal system (Chiapas, México) in

Rouwet, D.; Bellomo, S.; Brusca, L.; Inguaggiato, S.; Jutzeler, M.; Mora, R.; Mazot, A.; Bernard, R.; Cassidy, M.; Taran, Y.

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Geofísica Internacional
Repositorio
Revistas UNAM
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Rouwet, D., et al. (2009). Major and trace element geochemistry of El Chichón volcano-hydrothermal system (Chiapas, México) in. Geofísica Internacional; Vol. 48 Núm. 1: Enero 1, 2009; 55-72. Recuperado de https://repositorio.unam.mx/contenidos/4132296

Descripción del recurso

Autor(es)
Rouwet, D.; Bellomo, S.; Brusca, L.; Inguaggiato, S.; Jutzeler, M.; Mora, R.; Mazot, A.; Bernard, R.; Cassidy, M.; Taran, Y.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Major and trace element geochemistry of El Chichón volcano-hydrothermal system (Chiapas, México) in
Fecha
2009-01-01
Resumen
Isotopic, major and trace element composition studies for the crater lake, the Soap Pool and thermal springs at El Chichón volcano in November 2006-October 2007 confirm the complex relationship between annual rainfall distribution and crater lake volume and chemistry. In 2001, 2004 and 2007 high volume high-Cl lake may be related to reactivation of high discharge (>10 kg/s) saline near-neutral water from the Soap Pool boiling springs into the lake, a few months (~January) after the end of the rainy season (June-October). The peak lake volume occurred in March 2007 (~6 x 105 m3). Agua Tibia 2 thermal springs discharge near the foot of the SW dome but their chemistry suggests a lower temperature regime, an enhanced water-rock interaction and basement contribution (evaporites and carbonates), anhydrite leaching from the 1982 pyroclastic deposits, rather than dome activity. New suggestions of crater lake seepage are evidenced by the Agua Caliente thermal springs. Existing models on the “crater lake-Soap Pool spring” and the deep hydrothermal system are discussed. Chemical changes in the deep geothermal aquifer feeding the thermal springs may predict dome rise. Future volcanic surveillance should focus on spring chemistry variations, as well as crater lake monitoring.doi: https://doi.org/10.22201/igeof.00167169p.2009.48.1.99
Tema
El Chichón; geoquímica de fluidos; monitoreo volcánico; El Chichón; fluid geochemistry; volcanic surveillance
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces