dor_id: 4133106

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

590.#.#.c: Open Journal Systems (OJS)

270.#.#.d: MX

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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/449/464

100.1.#.a: Rabeh, Taha

524.#.#.a: Rabeh, Taha (2012). Looking for active faults at east Qattara depression, northwestern desert, Egypt. Geofísica Internacional; Vol. 51 Núm. 4: Octubre 1, 2012; 323-­337. Recuperado de https://repositorio.unam.mx/contenidos/4133106

245.1.0.a: Looking for active faults at east Qattara depression, northwestern desert, Egypt

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2012

264.#.1.c: 2012-10-01

653.#.#.a: prospección magnetica; líneas sísmicas; estructuras del subsuelo; magnetic survey; seismic lines; subsurface structures

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/449

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/449

041.#.7.h: spa

520.3.#.a: Potential field methods are considered the cheapest tools in geophysical exploration to detect and characterize subsurface structures. Here we present a detailed land magnetic survey in an East Qattara Depression that was subjected before to a reflection seismic investigation. The main target of this study is infer the deeper subsurface structures and to investigate possible relations of these structures with earthquake activity. The reduced to north Pole (RTP) aeromagnetic map was used for detecting the regional extension of the interpreted structures on the land magnetic survey. The interpretations were performed on the RTP land and aeromagnetic maps using filtering techniques, least squares separations, tectonic trend analysis, spectral analysis, Werner and Euler deconvolutions, and 2.5­D modelling techniques. The results indicate that the main dominant tectonic trends are N35°Â­ 45°W, N45°Â­65°E, E­W and Aqaba trends. Moreover two seismic lines WQ85­31B and 127 were interpreted and compared with the deduced tectonic map. The results show that there is a great correlation between the location of the faults deduced from both the magnetic and seismic data. The results agree with the well logging data. Furthermore these structures correlated with the recorded earthquake activity by the National Egyptian Seismological Network (ENSN). This correlation implies that the studied area is more stable than other adjacent areas in the northern parts of Egypt close to the Mediterranean Sea and the Nile Delta River.doi: https://doi.org/10.22201/igeof.00167169p.2012.51.4.1229

773.1.#.t: Geofísica Internacional; Vol. 51 Núm. 4: Octubre 1, 2012; 323-­337

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: 323-­337

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

doi: https://doi.org/10.22201/igeof.00167169p.2012.51.4.1229

handle: 522ded443b037158

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

856.#.0.q: application/pdf

file_creation_date: 2022-07-06 17:15:08.0

file_modification_date: 2022-07-06 17:15:08.0

file_creator: Taha Rabeh

file_name: a031784b49b785c05cc43b01a0d2b924a2a2e9373c29d03c544d136f59e66d69.pdf

file_pages_number: 15

file_format_version: application/pdf; version=1.6

file_size: 1620779

245.1.0.b: Looking for active faults at east Qattara depression, northwestern desert, Egypt

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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Artículo

Looking for active faults at east Qattara depression, northwestern desert, Egypt

Rabeh, Taha

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

Rabeh, Taha (2012). Looking for active faults at east Qattara depression, northwestern desert, Egypt. Geofísica Internacional; Vol. 51 Núm. 4: Octubre 1, 2012; 323-­337. Recuperado de https://repositorio.unam.mx/contenidos/4133106

Descripción del recurso

Autor(es)
Rabeh, Taha
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Looking for active faults at east Qattara depression, northwestern desert, Egypt
Fecha
2012-10-01
Resumen
Potential field methods are considered the cheapest tools in geophysical exploration to detect and characterize subsurface structures. Here we present a detailed land magnetic survey in an East Qattara Depression that was subjected before to a reflection seismic investigation. The main target of this study is infer the deeper subsurface structures and to investigate possible relations of these structures with earthquake activity. The reduced to north Pole (RTP) aeromagnetic map was used for detecting the regional extension of the interpreted structures on the land magnetic survey. The interpretations were performed on the RTP land and aeromagnetic maps using filtering techniques, least squares separations, tectonic trend analysis, spectral analysis, Werner and Euler deconvolutions, and 2.5­D modelling techniques. The results indicate that the main dominant tectonic trends are N35°Â­ 45°W, N45°Â­65°E, E­W and Aqaba trends. Moreover two seismic lines WQ85­31B and 127 were interpreted and compared with the deduced tectonic map. The results show that there is a great correlation between the location of the faults deduced from both the magnetic and seismic data. The results agree with the well logging data. Furthermore these structures correlated with the recorded earthquake activity by the National Egyptian Seismological Network (ENSN). This correlation implies that the studied area is more stable than other adjacent areas in the northern parts of Egypt close to the Mediterranean Sea and the Nile Delta River.doi: https://doi.org/10.22201/igeof.00167169p.2012.51.4.1229
Tema
prospección magnetica; líneas sísmicas; estructuras del subsuelo; magnetic survey; seismic lines; subsurface structures
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces