dor_id: 4132257

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/478/492

100.1.#.a: Khutorskoyt, M. D.; Delgado-argotez, L. A.; Fernández, R.; Kononovt, V. I.; Polyakt, B. G.

524.#.#.a: Khutorskoyt, M. D., et al. (1994). Tectonic of the offshore Manzanillo and Tecpan basins, Mexican Pacific, from heat flow, bathymetric and seismic data. Geofísica Internacional; Vol. 33 Núm. 1: Enero 1, 1994; 161-185. Recuperado de https://repositorio.unam.mx/contenidos/4132257

245.1.0.a: Tectonic of the offshore Manzanillo and Tecpan basins, Mexican Pacific, from heat flow, bathymetric and seismic data

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: México; Cuenca de Manzanillo; Tecpan; Bloque Jalisco; Trinchera Mesoamericana; flujo de calor; perfiles sísmicos de reflexión; batimetría; Mexico; Manzanillo Basin; Tecpan; Jalisco Block; Middle American Trench; heat flow; seismic reflection profiles; bathymetry

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/478

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/478

041.#.7.h: spa

520.3.#.a: Separation of the Jalisco Block has been proposed to be the main results of oblique differential subduction of the Rivera and Cocos plates beneath North America and of the interaction between the four plates. Vector analysis of the subduction process of the Rivera and Cocos plates relative to North America results in a N11°E trending strike-slip fault boundary between the oceanic plates (at 4.2 cm/yr). most of the onshore structures are in the range of N30°-40°E and N60°-70°E, as in the Tecpan area (between Zihuatanejo and Acapulco). These results agree with the interoperation of detailed marine geophysical data collected by the R/V "Akademik Nikolai Strakhov" during February-March 1989 off Manzanillo and Tecpan. The data include seismic reflection profiles, swath bathymetric data, and 122 new direct heat flow data. Also 39 indirect heat flow values were estimated based on location of gas-hydratelayers in the Manzanillo continental slope from seismic records. In the Manzanillo Basin seismic profiling and swath bathymetric data indicate a recent uplift associated with strike-slip faulting. Heat flow ranges between 20-35 mW/m2. (average of 28±6 mW/m2) in the western Manzanillo Basin and 51±7 mW/m2 in the eastern basin. Both areas are bound by strike-slip faulting with a vertical component. The low heat flow is attributed to a portion of the coastal batholith that may have moved seaward along left-lateral faults in the Jalisco Block. The average heat flow value in the eastern portion is typical of the continental slope of the Middle American Trench; as measure off Tecpan, Guerrero, at an average of 55±8 mW/m2. High heat flow (>100 mW/m2) was found on the oceanic slope of the Middle American Trench. It is attributed to the younger age of the oceanic crust and/or to surface hydrothermal and local magmatic sources in the area of the El Gordo Graben.doi: https://doi.org/10.22201/igeof.00167169p.1994.33.1.547

773.1.#.t: Geofísica Internacional; Vol. 33 Núm. 1: Enero 1, 1994; 161-185

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: 161-185

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

doi: https://doi.org/10.22201/igeof.00167169p.1994.33.1.547

handle: 00db6c906fc02843

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

856.#.0.q: application/pdf

file_creation_date: 2008-02-22 16:47:27.0

file_modification_date: 2022-07-05 18:14:11.0

file_creator: M.D. Khutorskoyt

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245.1.0.b: Tectonic of the offshore Manzanillo and Tecpan basins, Mexican Pacific, from heat flow, bathymetric and seismic data

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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