dor_id: 4133373

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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

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100.1.#.a: Murray, J. B.

524.#.#.a: Murray, J. B. (1993). Ground deformation at Colima Volcano, Mexico, 198. Geofísica Internacional; Vol. 32 Núm. 4: Octubre 1, 1993; 659-669. Recuperado de https://repositorio.unam.mx/contenidos/4133373

245.1.0.a: Ground deformation at Colima Volcano, Mexico, 198

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1993

264.#.1.c: 1993-10-01

653.#.#.a: Deformación; Inclinometría seca; Subsidencia; Ground deformation; Levelling, Dry tilt; Subsidence

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001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1408

041.#.7.h: spa

520.3.#.a: A ground deformation network, now comprising I 0 Km of levelling traverse and six dry tilt stations, has been measured four times since it was first set up at Colima Volcano by the author in 1982. The results show continuous subsidence roughly centred around the summit area, together with a progressive tilt towards the south or southwest. The rate of subsidence averages about 0.4 em per km each year, though higher rates (around 1 em per km per year) were measured between 1982-86, and again in 1990-91, in the build up to the 1991 increase in activity. Simple elastic models filled to the levelling data are (consistcnt with the deflation of a buried source at 2 to 4 km depth, perhaps a draining magma chamber or the top of a magmatic column. The dry tilt results confirm the subsidence and its variable rate, although parallel tilts often occur in the overall downslope direction, suggesting gravitational creep or sliding of the volcano downslope.doi: https://doi.org/10.22201/igeof.00167169p.1993.32.4.610

773.1.#.t: Geofísica Internacional; Vol. 32 Núm. 4: Octubre 1, 1993; 659-669

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doi: https://doi.org/10.22201/igeof.00167169p.1993.32.4.610

handle: 24f331794f3291af

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

856.#.0.q: application/pdf

file_creation_date: 2008-03-25 16:06:06.0

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file_creator: J.B. Murray

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245.1.0.b: Ground deformation at Colima Volcano, Mexico, 1982 to 1991

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

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Artículo

Ground deformation at Colima Volcano, Mexico, 198

Murray, J. B.

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
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Murray, J. B. (1993). Ground deformation at Colima Volcano, Mexico, 198. Geofísica Internacional; Vol. 32 Núm. 4: Octubre 1, 1993; 659-669. Recuperado de https://repositorio.unam.mx/contenidos/4133373

Descripción del recurso

Autor(es)
Murray, J. B.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Ground deformation at Colima Volcano, Mexico, 198
Fecha
1993-10-01
Resumen
A ground deformation network, now comprising I 0 Km of levelling traverse and six dry tilt stations, has been measured four times since it was first set up at Colima Volcano by the author in 1982. The results show continuous subsidence roughly centred around the summit area, together with a progressive tilt towards the south or southwest. The rate of subsidence averages about 0.4 em per km each year, though higher rates (around 1 em per km per year) were measured between 1982-86, and again in 1990-91, in the build up to the 1991 increase in activity. Simple elastic models filled to the levelling data are (consistcnt with the deflation of a buried source at 2 to 4 km depth, perhaps a draining magma chamber or the top of a magmatic column. The dry tilt results confirm the subsidence and its variable rate, although parallel tilts often occur in the overall downslope direction, suggesting gravitational creep or sliding of the volcano downslope.doi: https://doi.org/10.22201/igeof.00167169p.1993.32.4.610
Tema
Deformación; Inclinometría seca; Subsidencia; Ground deformation; Levelling, Dry tilt; Subsidence
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces