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336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

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100.1.#.a: Takahashi, Masaki

524.#.#.a: Takahashi, Masaki (1994). Miocene tectonic deformation of central Japan-Paleomagnetic evidence of intra-arc bending. Geofísica Internacional; Vol. 33 Núm. 1: Enero 1, 1994; 25-44. Recuperado de https://repositorio.unam.mx/contenidos/4132721

245.1.0.a: Miocene tectonic deformation of central Japan-Paleomagnetic evidence of intra-arc bending

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: Rotación tectónica; tectónica de collision; paleomagnetismo; islas Japonesas; tectónica de arco de islas; Tectonic rotation; collision tectonics; paleomagnetism; Japanese Islands; island arc tectonics

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

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041.#.7.h: spa

520.3.#.a: Recent paleomagnetic studies in the Kanto Mountains, central Japan, have revealed Miocene rotation of the east-wing of the bending structure of pre-Neogene geologic terranes. More than 90° colckwise rotation of the Kanto Mountains took place between 15 and 6 Ma. In contrast, Southwest Japan and it eastern part (Nohi area) have rotate clockwise through 47° and 13-17° around 15 Ma, respectively. This differential rotation represents an intra-arc deformation during the Miocene. In addition, the field investigations reveal that the Izu-Bonin arc has been colliding with central Japan since the Middle Miocene. Along whit this previous paleomagnetic results accompanied with geological studies in central Japan, it is concluded that lateral bending of central Japan occurred during 15 and 16 Ma in association with the collision between the southeastward drifting Japanese Islands and the northwestward migrating Izu-Bonin arc.doi: https://doi.org/10.22201/igeof.00167169p.1994.33.1.538

773.1.#.t: Geofísica Internacional; Vol. 33 Núm. 1: Enero 1, 1994; 25-44

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

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300.#.#.a: Páginas: 25-44

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

doi: https://doi.org/10.22201/igeof.00167169p.1994.33.1.538

handle: 1ab1d326dc0c6f3a

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

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file_modification_date: 2022-07-05 20:40:49.0

file_creator: Masaki Takahashi

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245.1.0.b: Miocene tectonic deformation of central Japan-Paleomagnetic evidence of intra-arc bending

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

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Artículo

Miocene tectonic deformation of central Japan-Paleomagnetic evidence of intra-arc bending

Takahashi, Masaki

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

Takahashi, Masaki (1994). Miocene tectonic deformation of central Japan-Paleomagnetic evidence of intra-arc bending. Geofísica Internacional; Vol. 33 Núm. 1: Enero 1, 1994; 25-44. Recuperado de https://repositorio.unam.mx/contenidos/4132721

Descripción del recurso

Autor(es)
Takahashi, Masaki
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Miocene tectonic deformation of central Japan-Paleomagnetic evidence of intra-arc bending
Fecha
1994-01-01
Resumen
Recent paleomagnetic studies in the Kanto Mountains, central Japan, have revealed Miocene rotation of the east-wing of the bending structure of pre-Neogene geologic terranes. More than 90° colckwise rotation of the Kanto Mountains took place between 15 and 6 Ma. In contrast, Southwest Japan and it eastern part (Nohi area) have rotate clockwise through 47° and 13-17° around 15 Ma, respectively. This differential rotation represents an intra-arc deformation during the Miocene. In addition, the field investigations reveal that the Izu-Bonin arc has been colliding with central Japan since the Middle Miocene. Along whit this previous paleomagnetic results accompanied with geological studies in central Japan, it is concluded that lateral bending of central Japan occurred during 15 and 16 Ma in association with the collision between the southeastward drifting Japanese Islands and the northwestward migrating Izu-Bonin arc.doi: https://doi.org/10.22201/igeof.00167169p.1994.33.1.538
Tema
Rotación tectónica; tectónica de collision; paleomagnetismo; islas Japonesas; tectónica de arco de islas; Tectonic rotation; collision tectonics; paleomagnetism; Japanese Islands; island arc tectonics
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces