dor_id: 4133173

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/448/462

100.1.#.a: Ochoa-gonzález, Gil Humberto; Carreón-freyre, Dora; Cerca, Mariano; López-martínez, Margarita

524.#.#.a: Ochoa-gonzález, Gil Humberto, et al. (2015). Assessment of groundwater flow in volcanic faulted areas. A study case in Queretaro, Mexico. Geofísica Internacional; Vol. 54 Núm. 3: Julio 1, 2015; 199-220. Recuperado de https://repositorio.unam.mx/contenidos/4133173

245.1.0.a: Assessment of groundwater flow in volcanic faulted areas. A study case in Queretaro, Mexico

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2015

264.#.1.c: 2015-07-01

653.#.#.a: Flujo de aguas subterráneas; sistema acuífero fallado; modelación numérica; estructuras volcánicas; diques; México; Groundwater flow; faulted aquifers; numerical modeling; volcanic structures; dykes; Mexicos

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/448

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/448

041.#.7.h: spa

520.3.#.a: This work integrates local stratigraphy and faults to constraint a numerical model of groundwater flow in the North area of the Valley of Queretaro aquifer. Basic geological information was established from the reinterpretation of well logs, 40Ar*/39Ar dating of rocks, and field mapping. In particular, dating allowed to obtain the timing of emplacement of a magmatic dyke inferred to be emplaced along the El Nabo fault. The increase of flow rate and temperature in the El Nabo well suggest that the fault and dike transport a regional flow. A numerical model was implemented to evaluate the contributions of faulting and volcanic structures in the overall groundwater flow. The model, accomplished with the Visual-Modflow software and Modflow 2000 code, was partially constrained by the results of a pumping test in the El Nabo well, the deepest well (Lat. 20°42"14"N, Long. 100°28"45"W, ca. 1000 m depth) located in the Queretaro area. The interpretation of the model results and field observations suggest that faults collect the regional flow, compartmentalize the reservoir, and are responsible of the dramatic increase of flow rate from 6 to 47 l/s when drilling the El Nabo well below a depth of 850 m. The study presented here allowed the assessment of normal faults and intrusives determining groundwater flow and might be relevant to the knowledge of flow dynamics in nearby volcanic valleys. The analysis of the pumping test suggest the presence of two different groundwater flow systems: (1) a flow related with the limestone and shale unit and (2) a regional linear flow through faults. The implemented numerical model, based on geological information, allowed a better understanding of complex aquifer systems that cannot be evaluated by analytical methods. Moreover it can be a useful application for a better interpretation of pumping tests and to add complementary data of other pumping tests and/or hydrogeochemical analysis.doi: https://doi.org/10.1016/j.gi.2015.04.016

773.1.#.t: Geofísica Internacional; Vol. 54 Núm. 3: Julio 1, 2015; 199-220

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: 199-220

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

doi: https://doi.org/10.1016/j.gi.2015.04.016

handle: 00903f372e97fced

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

856.#.0.q: application/pdf

file_creation_date: 2017-04-07 17:02:09.0

file_modification_date: 2022-07-05 21:10:30.0

file_creator: Ochoa-González G.H.

file_name: 406ceb367bf7949c36f4efaf15a760bcd32096cc4819d9dab1b70812622ae2a5.pdf

file_pages_number: 22

file_format_version: application/pdf; version=1.4

file_size: 6993692

245.1.0.b: Assessment of groundwater flow in volcanic faulted areas. A study case in Queretaro, Mexico

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