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
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
590.#.#.c: Open Journal Systems (OJS)
270.#.#.d: MX
270.1.#.d: México
590.#.#.b: Concentrador
883.#.#.u: https://revistas.unam.mx/catalogo/
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/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
file_name: 6778d8321d8694f6297bccd094e9633abf6a0e1db8c685f926a072b3cc38b924.pdf
file_pages_number: 18
file_format_version: application/pdf; version=1.3
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
license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es
license_type: by-nc-sa
No entro en nada
No entro en nada 2