dor_id: 4133464

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/196/186

100.1.#.a: Abou-deeb, J. M.; Tarling, D. H.

524.#.#.a: Abou-deeb, J. M., et al. (2005). A palaeomagnetic study of Upper Pliocene volcanic rocks in the area of the Levant Fault near Homs, western Syria. Geofísica Internacional; Vol. 44 Núm. 3: Julio 1, 2005; 221-230. Recuperado de https://repositorio.unam.mx/contenidos/4133464

245.1.0.a: A palaeomagnetic study of Upper Pliocene volcanic rocks in the area of the Levant Fault near Homs, western Syria

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2005

264.#.1.c: 2005-07-01

653.#.#.a: Paleomagnetismo; rotaciones tectónicas; Falla Levante; Plioceno superior; Siria; Líbano; Palaeomagnetism; tectonic rotations; Levant Fault; Upper Pliocene; Syria; Lebanon

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/196

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/196

041.#.7.h: spa

520.3.#.a: Thermal demagnetisation of samples from 75 sites in basaltic rocks, mostly within 5 km of the Levant Fault, identifies consistent directions of remanence in most sites. Normal, Reversed and Intermediate polarities are identified, with Reversed polarities dominating. The Normal and Reversed sites are similarly magnetised, 5.6±5.3 A/m, while those of sites of Intermediate or undefined direction are somewhat more strongly magnetised, 11.9±9.5 A/m. The low field susceptibilities are consistent, 30.9±15.2 mSI, implying the geomagnetic field may have been somewhat stronger than during Normal or Reversed polarity. When the mean directions of the Normal sites are reversed, all sites have similar mean inclination values, 48.2° (δInc. = 2.7°), but the site mean declinations show a regional pattern. Sites from the 3 regions west of the Levant Fault zone (Marmarita, Qalat El-Hossen, Tel Kalakh) have similar declinations, 186° (δDec. = 5.4°). These are consistent with those from the Sufer and E. Ain Kut regions, 197° (δDec. = 3.9°), furthest east of the Levant Fault zone. All these localities have directions that are consistent with those expected for this part of Arabia for this time. However, all sites east and close to the Levant Fault zone (Bahur, W. Ain-Kut, Mzeineh and Buqeia) have more eastern declinations, averaging 154.0±12.0°. The declination difference, 37.3°, indicates the presence of rotated blocks adjacent to the eastern side of the Levant Fault. Such a rotation is consistent with the 25 km displace-ment predicted for this location and appears consistent with the subsequent volcanological and tectonic evolution of the Levant Fault, suggesting significant rotation and seismic activity during the last 5 Ma.doi: https://doi.org/10.22201/igeof.00167169p.2005.44.3.194

773.1.#.t: Geofísica Internacional; Vol. 44 Núm. 3: Julio 1, 2005; 221-230

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: 221-230

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

doi: https://doi.org/10.22201/igeof.00167169p.2005.44.3.194

handle: 1342a5164aa290a7

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

856.#.0.q: application/pdf

file_creation_date: 2005-11-21 19:11:44.0

file_modification_date: 2022-05-23 19:04:06.0

file_creator: Abou-Deeb J.M.

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245.1.0.b: A palaeomagnetic study of Upper Pliocene volcanic rocks in the area of the Levant Fault near Homs, western Syria

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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