dor_id: 4132813

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/642/648

100.1.#.a: Alcántara-ayala, Irasema

524.#.#.a: Alcántara-ayala, Irasema (1999). The Torvizcón, Spain, landslide of February 1996: the role of lithology in a semi-arid climate. Geofísica Internacional; Vol. 38 Núm. 3: Julio 1, 1999; 175-184. Recuperado de https://repositorio.unam.mx/contenidos/4132813

245.1.0.a: The Torvizcón, Spain, landslide of February 1996: the role of lithology in a semi-arid climate

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1999

264.#.1.c: 1999-07-01

653.#.#.a: deslizamientos superficiales; terrenos metamórficos; modelo infinito de ladera; análisis retrospectivo; análisis de sensitividad; Shallow failures; metamorphic terrains; infinite slope model; back analysis; sensitivity analysis

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/642

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/642

041.#.7.h: spa

520.3.#.a: The analysis of a shallow landslide in las Alpujarras, a metamorphic terrain of semi-arid Spain is presented. The extensive outcropping of phyllites and mica-schist is one of the most important keys in the understanding of mass failure. The degree of schistosity offers planes of weakness where water can penetrate and cause mass movement processes by increasing pore water pressures. A shallow slope movement occurred during extreme events, causing damage to the local and regional infrastructure and increasing the likelihood of natural disasters. By using the infinite slope model of Skempton and DeLory, a back analysis of an observed shallow landslide was carried out. The results of the sensitivity analysis indicated that material properties play a signifi- cant role in controlling slope processes and that the slope angle should not be considered as the only parameter to define instability threshold.doi: https://doi.org/10.22201/igeof.00167169p.1999.38.3.380

773.1.#.t: Geofísica Internacional; Vol. 38 Núm. 3: Julio 1, 1999; 175-184

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: 175-184

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

doi: https://doi.org/10.22201/igeof.00167169p.1999.38.3.380

handle: 0dc9cc0502d2a77b

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

856.#.0.q: application/pdf

file_creation_date: 2000-02-17 13:33:35.0

file_modification_date: 2022-07-12 17:35:47.0

file_creator: Irasema Alcántara-Ayala

file_name: 66d38e87f1a1f652a6625126e3b7c2dba91e0817bae7c1de2161a3737a4a569f.pdf

file_pages_number: 10

file_format_version: application/pdf; version=1.6

file_size: 380606

245.1.0.b: The Torvizcón, Spain, landslide of February 1996: the role of lithology in a semi-arid climate

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

No entro en nada

No entro en nada 2

Artículo

The Torvizcón, Spain, landslide of February 1996: the role of lithology in a semi-arid climate

Alcántara-ayala, Irasema

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

Alcántara-ayala, Irasema (1999). The Torvizcón, Spain, landslide of February 1996: the role of lithology in a semi-arid climate. Geofísica Internacional; Vol. 38 Núm. 3: Julio 1, 1999; 175-184. Recuperado de https://repositorio.unam.mx/contenidos/4132813

Descripción del recurso

Autor(es)
Alcántara-ayala, Irasema
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
The Torvizcón, Spain, landslide of February 1996: the role of lithology in a semi-arid climate
Fecha
1999-07-01
Resumen
The analysis of a shallow landslide in las Alpujarras, a metamorphic terrain of semi-arid Spain is presented. The extensive outcropping of phyllites and mica-schist is one of the most important keys in the understanding of mass failure. The degree of schistosity offers planes of weakness where water can penetrate and cause mass movement processes by increasing pore water pressures. A shallow slope movement occurred during extreme events, causing damage to the local and regional infrastructure and increasing the likelihood of natural disasters. By using the infinite slope model of Skempton and DeLory, a back analysis of an observed shallow landslide was carried out. The results of the sensitivity analysis indicated that material properties play a signifi- cant role in controlling slope processes and that the slope angle should not be considered as the only parameter to define instability threshold.doi: https://doi.org/10.22201/igeof.00167169p.1999.38.3.380
Tema
deslizamientos superficiales; terrenos metamórficos; modelo infinito de ladera; análisis retrospectivo; análisis de sensitividad; Shallow failures; metamorphic terrains; infinite slope model; back analysis; sensitivity analysis
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces