dor_id: 4132938

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

270.1.#.d: México

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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/1351/1333

100.1.#.a: Urrutia-fucugauchi, J.

524.#.#.a: Urrutia-fucugauchi, J. (1992). Reconnaissance electrical resistivity and self-potential studies of the Atotonilco-Jonacatepec region, Morelos State, Mexico.. Geofísica Internacional; Vol. 31 Núm. 4: Octubre 1, 1992; 341-358. Recuperado de https://repositorio.unam.mx/contenidos/4132938

245.1.0.a: Reconnaissance electrical resistivity and self-potential studies of the Atotonilco-Jonacatepec region, Morelos State, Mexico.

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1992

264.#.1.c: 1992-10-01

653.#.#.a: Sondeos de resistividad; Potencial natural; Estado de Morelos; Energía geotérmica; México; Resistivity soundings; Self-potential; Morelos State; Geothermal energy; Mexico

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/1351

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1351

041.#.7.h: spa

520.3.#.a: Preliminary results of a geophysical study of the Atotonilco-Jonacatepec area (Morelos State) using DC-resistivity and self-potential (SP) soundings, are used to outline the shallow underground structure of the volcanoclastic and lahar units and the intrusive bodies. Fifty-one 300 to 440 m-AB, six 600 m-AB and ten 1000 m-AB vertical soundings with the Schlumberger configuration were completed along three profiles. Most of the soundings could be interpreted by 3 to 4 layer models, but half of the 1000 m-AB soundings suggest more complex (multi-layered) structures. Maximum depths are of 150 to 250 meters. Deeper layers 4 and 5 may correspond to limestone; layers 2 and 3 may correspond to lahar deposits and sediments of the Tlayecac and Cayuca formations; and the surficial layer corresponds to unconsolidated material. The subsurface continuation of the Jantetelco granodiorites seems to be deeper than 150 meters. The SP anomalies are negative and appear to form part of larger dipolar anomalies. They may result from upwelling where regional southward flow approaches the intrusive bodies. Limited studies conducted over a limestone cave near Cocoyoc feature high apparent resistivities, which outline the surface projection of the cave entrance; parts of the cave deeper than 3-4 m proved difficult to detect. Soundings in a fault zone near Cafion de Lobos above volcanoclastic and alluvial sediments feature very low resistivities and almost flat Schlumberger apparent resistivity curves.

773.1.#.t: Geofísica Internacional; Vol. 31 Núm. 4: Octubre 1, 1992; 341-358

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: 341-358

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

doi: https://doi.org/10.22201/igeof.00167169p.1992.31.4.1351

handle: 2e94723b91329e96

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

856.#.0.q: application/pdf

file_creation_date: 2022-07-05 08:45:20.0

file_modification_date: 2022-07-26 01:07:48.0

file_creator: J. Urrutia-Fucugauchi

file_name: 01ffc3de4a21c1eedec4022ffa689accc00fc9a6619b6b19a5baf2dc69923a32.pdf

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245.1.0.b: Reconnaissance electrical resistivity and self-potential studies of the Atotonilco-Jonacatepec region, Morelos State, Mexico.

last_modified: 2023-06-20 16:00:00

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Artículo

Reconnaissance electrical resistivity and self-potential studies of the Atotonilco-Jonacatepec region, Morelos State, Mexico.

Urrutia-fucugauchi, J.

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

Urrutia-fucugauchi, J. (1992). Reconnaissance electrical resistivity and self-potential studies of the Atotonilco-Jonacatepec region, Morelos State, Mexico.. Geofísica Internacional; Vol. 31 Núm. 4: Octubre 1, 1992; 341-358. Recuperado de https://repositorio.unam.mx/contenidos/4132938

Descripción del recurso

Autor(es)
Urrutia-fucugauchi, J.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Reconnaissance electrical resistivity and self-potential studies of the Atotonilco-Jonacatepec region, Morelos State, Mexico.
Fecha
1992-10-01
Resumen
Preliminary results of a geophysical study of the Atotonilco-Jonacatepec area (Morelos State) using DC-resistivity and self-potential (SP) soundings, are used to outline the shallow underground structure of the volcanoclastic and lahar units and the intrusive bodies. Fifty-one 300 to 440 m-AB, six 600 m-AB and ten 1000 m-AB vertical soundings with the Schlumberger configuration were completed along three profiles. Most of the soundings could be interpreted by 3 to 4 layer models, but half of the 1000 m-AB soundings suggest more complex (multi-layered) structures. Maximum depths are of 150 to 250 meters. Deeper layers 4 and 5 may correspond to limestone; layers 2 and 3 may correspond to lahar deposits and sediments of the Tlayecac and Cayuca formations; and the surficial layer corresponds to unconsolidated material. The subsurface continuation of the Jantetelco granodiorites seems to be deeper than 150 meters. The SP anomalies are negative and appear to form part of larger dipolar anomalies. They may result from upwelling where regional southward flow approaches the intrusive bodies. Limited studies conducted over a limestone cave near Cocoyoc feature high apparent resistivities, which outline the surface projection of the cave entrance; parts of the cave deeper than 3-4 m proved difficult to detect. Soundings in a fault zone near Cafion de Lobos above volcanoclastic and alluvial sediments feature very low resistivities and almost flat Schlumberger apparent resistivity curves.
Tema
Sondeos de resistividad; Potencial natural; Estado de Morelos; Energía geotérmica; México; Resistivity soundings; Self-potential; Morelos State; Geothermal energy; Mexico
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces