dor_id: 4132712

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares

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

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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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883.#.#.a: Revistas UNAM

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

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/416/430

100.1.#.a: Terán-mendieta, Luis F.; Valenzuela Wong, Raúl

524.#.#.a: Terán-mendieta, Luis F., et al. (2012). Radial S wave velocity structure of the D” region under a spot of the D" region under a spot of the east central Pacific Ocean. Geofísica Internacional; Vol. 51 Núm. 3: Julio 1, 2012; 207-­224. Recuperado de https://repositorio.unam.mx/contenidos/4132712

245.1.0.a: Radial S wave velocity structure of the D” region under a spot of the D" region under a spot of the east central Pacific Ocean

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2012

264.#.1.c: 2012-07-01

653.#.#.a: ondas difractadas; interfaz nucleo-manto; D; constante de disipación; post-perovskita; capa térmica limítrofe; diffracted waves; core-mantle boundary; D; decay constant; post-perovskite; thermal boundary layer

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/416

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/416

041.#.7.h: spa

520.3.#.a: The S wave radial velocity structure at the base of the mantle was constrained for an area of the east central Pacific Ocean centered at 19°N, 132°W. The decay constant technique was applied in the frequency domain to the S and S<sub>diff</sub> waves of an earthquake in the Tonga Islands recorded in the northeastern United States. A total of 29 different S wave velocity models were explored, including models with a velocity discontinuity and also the Preliminary Reference Earth Model (PREM). As determined from the fit to the decay constant in the frequency domain and to the waveforms in the time domain, PREM was considered the best model. This choice implies that D" at this location is 150 km thick and has a slightly negative velocity gradient with increasing depth. No velocity discontinuity was found at the top of D". The proposed velocity structure is consistent with D" acting as a thermal boundary layer and also with the possible existence of mantle enriched in iron through chemical reactions with the core. The preferred model also implies the existence of slightly elevated temperatures at the base of the mantle. The lack of a discontinuity is consistent with the absence of subduction at this location during the last 180 Myr.doi: https://doi.org/10.22201/igeof.00167169p.2012.51.3.1193

773.1.#.t: Geofísica Internacional; Vol. 51 Núm. 3: Julio 1, 2012; 207-­224

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: 207-­224

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

doi: https://doi.org/10.22201/igeof.00167169p.2012.51.3.1193

handle: 3cb189c5ede90861

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

856.#.0.q: application/pdf

file_creation_date: 2022-07-05 18:21:39.0

file_modification_date: 2022-07-05 18:21:39.0

file_creator: Luis F. Terán-Mendieta

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file_pages_number: 18

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file_size: 668673

245.1.0.b: Radial S wave velocity structure of the D” region under a spot of the D" region under a spot of the east central Pacific Ocean

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

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Artículo

Radial S wave velocity structure of the D” region under a spot of the D" region under a spot of the east central Pacific Ocean

Terán-mendieta, Luis F.; Valenzuela Wong, Raúl

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

Terán-mendieta, Luis F., et al. (2012). Radial S wave velocity structure of the D” region under a spot of the D" region under a spot of the east central Pacific Ocean. Geofísica Internacional; Vol. 51 Núm. 3: Julio 1, 2012; 207-­224. Recuperado de https://repositorio.unam.mx/contenidos/4132712

Descripción del recurso

Autor(es)
Terán-mendieta, Luis F.; Valenzuela Wong, Raúl
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Radial S wave velocity structure of the D” region under a spot of the D" region under a spot of the east central Pacific Ocean
Fecha
2012-07-01
Resumen
The S wave radial velocity structure at the base of the mantle was constrained for an area of the east central Pacific Ocean centered at 19°N, 132°W. The decay constant technique was applied in the frequency domain to the S and S<sub>diff</sub> waves of an earthquake in the Tonga Islands recorded in the northeastern United States. A total of 29 different S wave velocity models were explored, including models with a velocity discontinuity and also the Preliminary Reference Earth Model (PREM). As determined from the fit to the decay constant in the frequency domain and to the waveforms in the time domain, PREM was considered the best model. This choice implies that D" at this location is 150 km thick and has a slightly negative velocity gradient with increasing depth. No velocity discontinuity was found at the top of D". The proposed velocity structure is consistent with D" acting as a thermal boundary layer and also with the possible existence of mantle enriched in iron through chemical reactions with the core. The preferred model also implies the existence of slightly elevated temperatures at the base of the mantle. The lack of a discontinuity is consistent with the absence of subduction at this location during the last 180 Myr.doi: https://doi.org/10.22201/igeof.00167169p.2012.51.3.1193
Tema
ondas difractadas; interfaz nucleo-manto; D; constante de disipación; post-perovskita; capa térmica limítrofe; diffracted waves; core-mantle boundary; D; decay constant; post-perovskite; thermal boundary layer
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces