dor_id: 4132113

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

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883.#.#.u: https://revistas.unam.mx/catalogo/

883.#.#.a: Revistas UNAM

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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/721/1199

100.1.#.a: Tsuchiya, Nobuyuki

524.#.#.a: Tsuchiya, Nobuyuki (1995). Middle Miocene rift magmatism of basaltic rocks in the Japan arc. Geofísica Internacional; Vol. 34 Núm. 3: Julio 1, 1995; 293-307. Recuperado de https://repositorio.unam.mx/contenidos/4132113

245.1.0.a: Middle Miocene rift magmatism of basaltic rocks in the Japan arc

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1995

264.#.1.c: 1995-07-01

653.#.#.a: Rift abortado; dique alimentador; subsidencia; extensión; basaltos de cuenca retro-arco; Japón; Failed rift; feeder dike; subsidence; extension; back-arc basin basalt; Japan

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/721

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/721

041.#.7.h: spa

520.3.#.a: Intense and widespread Middle Miocene basaltic magmatism occurred within and adjacent to the Akita-Yamagata oil field, located on the west flank of the NE Japan arc. This magmatism is distributed over a 200 km x 30 to 40 km area. Its estimated volume is 6,000 krn3, much larger than the 1,500 km3 estimated for the Quaternary volcanics in the NE Japan arc. It consists of extrusive and intrusive basaltic rocks that exhibit major and trace element compositions commonly associated with back-arc basin basalt. This composition suggests a mantle source with slight metasomatism by subduction components. The type of basaltic magmatism changed from extrusive to intrusive from early to late Middle Miocene. In early Middle Miocene, these rocks were extruded in an extensional tectonic environment, as feeder dykes trending NNE-SSW to NE-SW. The lava associated to this magmatism occurs intercalated with bathyal sediments and formed numerous submarine volcanoes. During the late Middle Miocene, basaltic rocks were mostly intruded into the sediments as dolerite sills. In the area surrounding the rift zone, widespread early Middle Miocene magmatism occurred in an extensional regime. This magmatism was bimodal, producing both acidic and basaltic rocks. The lava associated was subaerial and subaqueous (shallow water environment). We suggest that the rift zone is a failed continental rift possibly developed during the Middle Miocene along the periphery of the then actively spreading Japan Sea.

773.1.#.t: Geofísica Internacional; Vol. 34 Núm. 3: Julio 1, 1995; 293-307

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: 293-307

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

doi: https://doi.org/10.22201/igeof.00167169p.1995.34.3.721

handle: 7b8064716406593e

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

856.#.0.q: application/pdf

file_creation_date: 2022-07-07 11:45:53.0

file_modification_date: 2022-07-14 16:41:15.0

file_creator: Nobuyuki Tsuchiya

file_name: 1108c83089f712f60a682faf4377ea99bfc50007ac9f18b20ebd7e7832840320.pdf

file_pages_number: 16

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file_size: 2572397

245.1.0.b: Middle Miocene rift magmatism of basaltic rocks in the Japan arc

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

license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es

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Artículo

Middle Miocene rift magmatism of basaltic rocks in the Japan arc

Tsuchiya, Nobuyuki

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

Tsuchiya, Nobuyuki (1995). Middle Miocene rift magmatism of basaltic rocks in the Japan arc. Geofísica Internacional; Vol. 34 Núm. 3: Julio 1, 1995; 293-307. Recuperado de https://repositorio.unam.mx/contenidos/4132113

Descripción del recurso

Autor(es)
Tsuchiya, Nobuyuki
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Middle Miocene rift magmatism of basaltic rocks in the Japan arc
Fecha
1995-07-01
Resumen
Intense and widespread Middle Miocene basaltic magmatism occurred within and adjacent to the Akita-Yamagata oil field, located on the west flank of the NE Japan arc. This magmatism is distributed over a 200 km x 30 to 40 km area. Its estimated volume is 6,000 krn3, much larger than the 1,500 km3 estimated for the Quaternary volcanics in the NE Japan arc. It consists of extrusive and intrusive basaltic rocks that exhibit major and trace element compositions commonly associated with back-arc basin basalt. This composition suggests a mantle source with slight metasomatism by subduction components. The type of basaltic magmatism changed from extrusive to intrusive from early to late Middle Miocene. In early Middle Miocene, these rocks were extruded in an extensional tectonic environment, as feeder dykes trending NNE-SSW to NE-SW. The lava associated to this magmatism occurs intercalated with bathyal sediments and formed numerous submarine volcanoes. During the late Middle Miocene, basaltic rocks were mostly intruded into the sediments as dolerite sills. In the area surrounding the rift zone, widespread early Middle Miocene magmatism occurred in an extensional regime. This magmatism was bimodal, producing both acidic and basaltic rocks. The lava associated was subaerial and subaqueous (shallow water environment). We suggest that the rift zone is a failed continental rift possibly developed during the Middle Miocene along the periphery of the then actively spreading Japan Sea.
Tema
Rift abortado; dique alimentador; subsidencia; extensión; basaltos de cuenca retro-arco; Japón; Failed rift; feeder dike; subsidence; extension; back-arc basin basalt; Japan
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces