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
dor_id: 4132938
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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
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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
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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
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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
license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es
license_type: by-nc-sa
Urrutia-fucugauchi, J.
Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM
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