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100.1.#.a: Monterroso, David A.; Kulhánek, Ota

524.#.#.a: Monterroso, David A., et al. (2003). Spatial variations of b-values in the subduction zone of Central America. Geofísica Internacional; Vol. 42 Núm. 4: Octubre 1, 2003; 575-587. Recuperado de https://repositorio.unam.mx/contenidos/4132445

245.1.0.a: Spatial variations of b-values in the subduction zone of Central America

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

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264.#.0.c: 2003

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653.#.#.a: Valor de b; zona de subducción; América Central; cadena volcánica; esfuerzo; b-value; subduction zone; Central America; volcanic chain; stress

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520.3.#.a: Frequency-magnitude distribution along the Mid-American Trench (MAT) has been studied by means of 2345 earthquakes during the period 1964-1994. We used the regional MIDAS catalogue with a magnitude of completeness of 4.2. To resolve the b- value as a function of depth (one dimensional approach), we applied vertically sliding windows containing a constant number of events. To obtain more details in the b distribution, we projected catalogue hypocenters in three selected regions (approximately Guatemala and El Salvador, Nicaragua, Costa Rica), onto planes perpendicular to the trench. The b-values were calculated in sliding cylindrical volumes (two-dimensional approach) containing a constant number of earthquakes and centered at nodes of a 5 km x 5 km grid. The b-value varies significantly along a large part of MAT. High b-values were identified in the upper part of the slab at depths of 80-110 km beneath Guatemala-El Salvador and at depths 130-170 km beneath Nicaragua. Anomalous (high) b- values in the lower part of the slab were located at depths of 50-90 km and 50-160 km beneath Guatemala-El Salvador and Nicaragua, respectively. Anomalies observed at the upper part of the slab may be related to dehydration and successive increase in pore pressure in the down-going lithosphere, which may generate volcanism above the anomalies in the upper part of the slab. Anomalies on the lower surface of the Wadati-Benioff zone are likely to be associated with high thermal gradients between the slab and mantle.doi: https://doi.org/10.22201/igeof.00167169p.2003.42.4.312

773.1.#.t: Geofísica Internacional; Vol. 42 Núm. 4: Octubre 1, 2003; 575-587

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doi: https://doi.org/10.22201/igeof.00167169p.2003.42.4.312

handle: 117ad8e9263673eb

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

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file_creator: David A. Monterroso and Ota Kulhánek

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245.1.0.b: Spatial variations of b-values in the subduction zone of Central America

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Artículo

Spatial variations of b-values in the subduction zone of Central America

Monterroso, David A.; Kulhánek, Ota

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

Monterroso, David A., et al. (2003). Spatial variations of b-values in the subduction zone of Central America. Geofísica Internacional; Vol. 42 Núm. 4: Octubre 1, 2003; 575-587. Recuperado de https://repositorio.unam.mx/contenidos/4132445

Descripción del recurso

Autor(es)
Monterroso, David A.; Kulhánek, Ota
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Spatial variations of b-values in the subduction zone of Central America
Fecha
2003-10-01
Resumen
Frequency-magnitude distribution along the Mid-American Trench (MAT) has been studied by means of 2345 earthquakes during the period 1964-1994. We used the regional MIDAS catalogue with a magnitude of completeness of 4.2. To resolve the b- value as a function of depth (one dimensional approach), we applied vertically sliding windows containing a constant number of events. To obtain more details in the b distribution, we projected catalogue hypocenters in three selected regions (approximately Guatemala and El Salvador, Nicaragua, Costa Rica), onto planes perpendicular to the trench. The b-values were calculated in sliding cylindrical volumes (two-dimensional approach) containing a constant number of earthquakes and centered at nodes of a 5 km x 5 km grid. The b-value varies significantly along a large part of MAT. High b-values were identified in the upper part of the slab at depths of 80-110 km beneath Guatemala-El Salvador and at depths 130-170 km beneath Nicaragua. Anomalous (high) b- values in the lower part of the slab were located at depths of 50-90 km and 50-160 km beneath Guatemala-El Salvador and Nicaragua, respectively. Anomalies observed at the upper part of the slab may be related to dehydration and successive increase in pore pressure in the down-going lithosphere, which may generate volcanism above the anomalies in the upper part of the slab. Anomalies on the lower surface of the Wadati-Benioff zone are likely to be associated with high thermal gradients between the slab and mantle.doi: https://doi.org/10.22201/igeof.00167169p.2003.42.4.312
Tema
Valor de b; zona de subducción; América Central; cadena volcánica; esfuerzo; b-value; subduction zone; Central America; volcanic chain; stress
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces