dor_id: 4133532

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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270.#.#.d: MX

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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/1326/1306

100.1.#.a: Stock, Stock

524.#.#.a: Stock, Stock (1989). Sequence and geochronology of Miocene rocks adjacent to the main gulf escarpment: southern Valle Chico, Baja California Norte, Mexico. Geofísica Internacional; Vol. 28 Núm. 5: Diciembre 31, 1989; 851-896. Recuperado de https://repositorio.unam.mx/contenidos/4133532

245.1.0.a: Sequence and geochronology of Miocene rocks adjacent to the main gulf escarpment: southern Valle Chico, Baja California Norte, Mexico

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1989

264.#.1.c: 1989-12-01

653.#.#.a: Valle Chico; Baja California Norte-México; Geocronología; Mioceno; Geochronology; Miocene; Valle Chico; Baja California Norte-Mexico

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/1326

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1326

041.#.7.h: spa

520.3.#.a: Geologic mapping and K/Ar dating of Tertiary rocks in NE BajaCalifornia, at latitude 300 30" N, reveal a history of volcanism from 20 Ma to at least 6 Ma. From 20 to 15 Ma, basalt, andesite and pyroclastic flows locally covered the Cretaceous and older batholithic and prebatholithic rocks. These deposits were followed by up to 300 m of additional pyroclastic flows, reworked tuff, basalt, sandstone and conglomerate. Subsequent eruptions between 11 and 6 Ma produced andesite to rhyolite flows and breccias. Eruptions at about 6 Ma covered the region with up to an additional 300 m of pyroclastic flows, ash fall deposits and welded vitric tuff. These units cap the high plateaus of the northwestern corner of the Puertecitos volcanic province. Local undated volcanic units may be younger than 6 Ma. The tilting, faulting and topographic relief associated with the Main Gulf Escarpment began developing sometime between 11 and 6 Ma; variations in thickness of the pre-II Ma units are not generally fault-related, although variations in thickness of the 6 Ma deposits arc. The alignment of four pre-6 Ma volcanic vents along a NNW trend parallel to the present escarpment suggests that ascent of the magmasmay have been structurally controlled by Late Miocene extensional faults.doi: https://doi.org/10.22201/igeof.00167169p.1989.28.5.1289

773.1.#.t: Geofísica Internacional; Vol. 28 Núm. 5: Diciembre 31, 1989; 851-896

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: 851-896

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

doi: https://doi.org/10.22201/igeof.00167169p.1989.28.5.1289

handle: 35a2acfc0428f78c

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

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file_creation_date: 2008-06-25 20:04:10.0

file_modification_date: 2022-07-20 11:38:03.0

file_creator: J.M. Stock

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245.1.0.b: Sequence and geochronology of Miocene rocks adjacent to the main gulf escarpment: southern Valle Chico, Baja California Norte, Mexico

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Artículo

Sequence and geochronology of Miocene rocks adjacent to the main gulf escarpment: southern Valle Chico, Baja California Norte, Mexico

Stock, Stock

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

Stock, Stock (1989). Sequence and geochronology of Miocene rocks adjacent to the main gulf escarpment: southern Valle Chico, Baja California Norte, Mexico. Geofísica Internacional; Vol. 28 Núm. 5: Diciembre 31, 1989; 851-896. Recuperado de https://repositorio.unam.mx/contenidos/4133532

Descripción del recurso

Autor(es)
Stock, Stock
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Sequence and geochronology of Miocene rocks adjacent to the main gulf escarpment: southern Valle Chico, Baja California Norte, Mexico
Fecha
1989-12-01
Resumen
Geologic mapping and K/Ar dating of Tertiary rocks in NE BajaCalifornia, at latitude 300 30" N, reveal a history of volcanism from 20 Ma to at least 6 Ma. From 20 to 15 Ma, basalt, andesite and pyroclastic flows locally covered the Cretaceous and older batholithic and prebatholithic rocks. These deposits were followed by up to 300 m of additional pyroclastic flows, reworked tuff, basalt, sandstone and conglomerate. Subsequent eruptions between 11 and 6 Ma produced andesite to rhyolite flows and breccias. Eruptions at about 6 Ma covered the region with up to an additional 300 m of pyroclastic flows, ash fall deposits and welded vitric tuff. These units cap the high plateaus of the northwestern corner of the Puertecitos volcanic province. Local undated volcanic units may be younger than 6 Ma. The tilting, faulting and topographic relief associated with the Main Gulf Escarpment began developing sometime between 11 and 6 Ma; variations in thickness of the pre-II Ma units are not generally fault-related, although variations in thickness of the 6 Ma deposits arc. The alignment of four pre-6 Ma volcanic vents along a NNW trend parallel to the present escarpment suggests that ascent of the magmasmay have been structurally controlled by Late Miocene extensional faults.doi: https://doi.org/10.22201/igeof.00167169p.1989.28.5.1289
Tema
Valle Chico; Baja California Norte-México; Geocronología; Mioceno; Geochronology; Miocene; Valle Chico; Baja California Norte-Mexico
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces