dor_id: 4132799

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/469/483

100.1.#.a: Sugiyama, Yuichi

524.#.#.a: Sugiyama, Yuichi (1994). Neotectonics of Southwest Japan due to the right-oblique subduction of the Philippine Sea plate. Geofísica Internacional; Vol. 33 Núm. 1: Enero 1, 1994; 53-76. Recuperado de https://repositorio.unam.mx/contenidos/4132799

245.1.0.a: Neotectonics of Southwest Japan due to the right-oblique subduction of the Philippine Sea plate

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1994

264.#.1.c: 1994-01-01

653.#.#.a: Línea Tectónica Media; cuenca del Nankai; subducción oblicua; placa del Mar de Filipinas; suroeste de Japón; unidad estructural; Median Tectonic Line; Nankai Trough; oblique subduction; Philippine Sea plate; Southwest Japan; structural unit

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/469

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/469

041.#.7.h: spa

520.3.#.a: The forearc region of Southwest Japan is divided into five equivalent regions called structural units. Each unit is 120 to 150 km long and composed of a forearc basin fringed by an inverted L-shaped structural high extending from each of five promontories on the Pacific coast to the outer ridge zone along the Nankai Trough. The structural units coincide, in both dimension and location, with the source areas of plate-boundary carthquakes caused by low-angle thrusts with a right-lateral component. The topographic and structural features of the unit also correspond to the pattenr of crustal movements associated with the earthquakes. Form these facts, it is concluded that the structural units have been formed fundamentally by accumulation of coseismic crustal movements. The second Paleo-Seto inland sea, which existed east of the present-day Seto sea in Pliocene to Middle Pleistocene time, was composed of three right-handed en echeleon basins elongated in the NE-SW direction oblique to the Median Tectonic Line. The paleogeographic evidence shows that the second Paleo-Seto inland sea was formed as a right-lateral shear zone in association with the right-lateral strike-slip faulting of the MTL in the same manner as the present Seto inland sea. These characteristic neotectonic movement in the forearc region and along the MTL are attributed to the right-oblique subduction of the Philippine Sea plate at the Nankai Trough since the earliest Pliocene about 5 Ma.doi: https://doi.org/10.22201/igeof.00167169p.1994.33.1.540

773.1.#.t: Geofísica Internacional; Vol. 33 Núm. 1: Enero 1, 1994; 53-76

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: 53-76

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

doi: https://doi.org/10.22201/igeof.00167169p.1994.33.1.540

handle: 2d84429595d0c24f

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

856.#.0.q: application/pdf

file_creation_date: 2008-02-22 16:52:44.0

file_modification_date: 2022-07-05 18:39:43.0

file_creator: Yuichi Sugiyama

file_name: ab4c56169f199d9d2f723d51b9325bd53482457c1ae4037db106b435858f1ae0.pdf

file_pages_number: 24

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245.1.0.b: Neotectonics of Southwest Japan due to the right-oblique subduction of the Philippine Sea plate

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

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