dor_id: 4132808

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/239/228

100.1.#.a: Azeglio, E. A.; Gimenez, M. E.; Introcaso, A.

524.#.#.a: Azeglio, E. A., et al. (2010). Interpretation of Las Salinas sedimentary basin - Argentina, based on integration of geological and geophysical data. Geofísica Internacional; Vol. 49 Núm. 4: Octubre 1, 2010; 225-244. Recuperado de https://repositorio.unam.mx/contenidos/4132808

245.1.0.a: Interpretation of Las Salinas sedimentary basin - Argentina, based on integration of geological and geophysical data

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2010

264.#.1.c: 2010-10-01

653.#.#.a: Modelo geológico-geofísico integrado; reinterpretación sísmica; inversión gravimétrica 3D; cuenca de Las Salinas; Argentina; Geological and geophysical integrated model; seismic reinterpretation; 3D gravimetric inversion; Las Salinas Basin; Argentina

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/239

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/239

041.#.7.h: spa

520.3.#.a: Las Salinas sedimentary basin is located at 31º S and 67º W approximately, in the central-western part of Argentina. Its dimensions are 100 km long, about 50 km wide, plus an average altitude of 500 m above sea level. The basin is situated among the mountain ranges of De la Huerta, Guayaguas and Las Quijadas to the west, and the ranges of Chepes, Ulapes and San Luis to the east, with a NW-SE orientation. Its surface is approximately 5,700 km2 with an average depth of 5 km increasing in a northerly direction. The southern part of the basin is separated from the Beazley basin by the buried San Pedro ridge. New gravimetric information and archive file data, density data (from wells) and seismic reinterpretation allowed us to obtain an integrated model, which involved: a) seismic basement situated at a depth of 3.5 km obtained from seismic reinterpretation; b) crystalline basement with an average depth of 5 km obtained from inverted gravimetric data; c) perimeter and internal faults system reaching 11 km in depth suggesting a listric type disposition in depth, thick-skinned type, obtained from 2-D seismic reinterpretation, spectral analysis technique and alignments obtained from Euler’s technique; d) succession of density data extracted from wells allowing us to perform a gravimetric inversion from Bouguer’s anomalies operating with variable density; e) a system of three asymmetric breached anticlines crossed by three systems of inverse faults and f) regional structure serving as evidence, permitting us to dimension the compressive framework to which the region has been subjected. Our purpose is that this well-defined integrated model will contribute to the search for further geological structures of economic interest.doi: https://doi.org/10.22201/igeof.00167169p.2010.49.4.131

773.1.#.t: Geofísica Internacional; Vol. 49 Núm. 4: Octubre 1, 2010; 225-244

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: 225-244

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

doi: https://doi.org/10.22201/igeof.00167169p.2010.49.4.131

handle: 009627dce6a151fd

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

856.#.0.q: application/pdf

file_creation_date: 2010-09-27 16:51:13.0

file_modification_date: 2022-05-31 18:44:27.0

file_creator: E. A. Azeglio

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245.1.0.b: Interpretation of Las Salinas sedimentary basin - Argentina, based on integration of geological and geophysical 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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