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336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

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351.#.#.b: Geofísica Internacional

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/185/171

100.1.#.a: Cotilla Rodríguez, Mario Octavio; Córdoba Barba, Diego; Herraiz Sarachaga, Miguel

524.#.#.a: Cotilla Rodríguez, Mario Octavio, et al. (2005). Main morphotectonic characteristics of Asturias, Spain. Geofísica Internacional; Vol. 44 Núm. 1: Enero 1, 2005; 65-101. Recuperado de https://repositorio.unam.mx/contenidos/4132747

245.1.0.a: Main morphotectonic characteristics of Asturias, Spain

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2005

264.#.1.c: 2005-01-01

653.#.#.a: Asturias; España; morfotectónica; Península Ibérica; Asturias; Spain; morphotectonics; Iberian Peninsula

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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520.3.#.a: Asturias is part of one of the four morphotectonic mesoblocks that make up the Northern macroblock (Number 9) of the Iberian plate. The framework of territorial regionalization was developed on the basis of the methodology of Rantsman (1979) using different geologic-geophysical and geomorphological methods. The territorial units (1 mountain mesoblock, 8 blocks, 208 microblocks and 668 nanoblocks), morphoalignments (quantity/order: 1/2, 1/3, 10/4, 35/5 and 77/6) and morphotectonic knots (quantity/order: 2/3, 11/4, 31/5 and 86/6) can be distinguished in the cartography of Asturias. The number of well defined morphostructures increases, significantly, from west to east. At the block level, a very well defined transverse differentiation of the territorial units and morphoalignments is noticeable. This differentiation is interpreted as an expression of the region"s lithospheric heterogeneity. There is a clear relationship between morphostructures and seismicity, especially with respect to the higher activity found in the blocks adjacent to Oviedo and the northern and eastern regions. The oceanic sector is decidedly seismically active.doi: https://doi.org/10.22201/igeof.00167169p.2005.44.1.553

773.1.#.t: Geofísica Internacional; Vol. 44 Núm. 1: Enero 1, 2005; 65-101

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: 65-101

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doi: https://doi.org/10.22201/igeof.00167169p.2005.44.1.553

handle: 00c7ce92b6669c36

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

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file_modification_date: 2022-05-30 18:31:01.0

file_creator: Cotilla Rodríguez M.O.

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245.1.0.b: Main morphotectonic characteristics of Asturias, Spain

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Artículo

Main morphotectonic characteristics of Asturias, Spain

Cotilla Rodríguez, Mario Octavio; Córdoba Barba, Diego; Herraiz Sarachaga, Miguel

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

Cotilla Rodríguez, Mario Octavio, et al. (2005). Main morphotectonic characteristics of Asturias, Spain. Geofísica Internacional; Vol. 44 Núm. 1: Enero 1, 2005; 65-101. Recuperado de https://repositorio.unam.mx/contenidos/4132747

Descripción del recurso

Autor(es)
Cotilla Rodríguez, Mario Octavio; Córdoba Barba, Diego; Herraiz Sarachaga, Miguel
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Main morphotectonic characteristics of Asturias, Spain
Fecha
2005-01-01
Resumen
Asturias is part of one of the four morphotectonic mesoblocks that make up the Northern macroblock (Number 9) of the Iberian plate. The framework of territorial regionalization was developed on the basis of the methodology of Rantsman (1979) using different geologic-geophysical and geomorphological methods. The territorial units (1 mountain mesoblock, 8 blocks, 208 microblocks and 668 nanoblocks), morphoalignments (quantity/order: 1/2, 1/3, 10/4, 35/5 and 77/6) and morphotectonic knots (quantity/order: 2/3, 11/4, 31/5 and 86/6) can be distinguished in the cartography of Asturias. The number of well defined morphostructures increases, significantly, from west to east. At the block level, a very well defined transverse differentiation of the territorial units and morphoalignments is noticeable. This differentiation is interpreted as an expression of the region"s lithospheric heterogeneity. There is a clear relationship between morphostructures and seismicity, especially with respect to the higher activity found in the blocks adjacent to Oviedo and the northern and eastern regions. The oceanic sector is decidedly seismically active.doi: https://doi.org/10.22201/igeof.00167169p.2005.44.1.553
Tema
Asturias; España; morfotectónica; Península Ibérica; Asturias; Spain; morphotectonics; Iberian Peninsula
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces