dor_id: 4132137

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/63/61

100.1.#.a: Canet Miquel, Carles; Franco, Sara I.; Morelos Rodríguez, Lucero; Rajabi, Abdorahman; Núñez Useche, Fernando

524.#.#.a: Canet Miquel, Carles, et al. (2021). Geological note and historical review of the Pathé geothermal zone, Hidalgo. Geofísica Internacional; Vol. 60 Núm. 3: Julio 1, 2021; 258-279. Recuperado de https://repositorio.unam.mx/contenidos/4132137

245.1.0.a: Geological note and historical review of the Pathé geothermal zone, Hidalgo

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2021

264.#.1.c: 2021-07-01

653.#.#.a: Joseph Burkart; José Guadalupe Aguilera Serrano; Faja Volcánica Transmexicana; alteración hidrotermal; caolín; fallas normales; Joseph Burkart; José Guadalupe Aguilera Serrano; Trans-Mexican Volcanic Belt; hydrothermal alteration; kaolin; normal faults

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/63

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/63

041.#.7.h: spa

520.3.#.a: The Pathé geothermal zone, in the central portion of the Trans-Mexican Volcanic Belt, attracted a variety of scientists and explorers since late 18th century. Joseph Burkart (1798-1870), a German mining engineer and a contemporary of Alexander von Humboldt (1769-1859), provided in 1836 a geological description of the zone because of which Pathé was the first geothermal system to be studied in Mexico under modern science principles. At the beginning of the 20th century, this zone was investigated by the Mexican geologist José Guadalupe Aguilera Serrano (1857-1941), who described in 1907 the local volcanic rocks and their alteration. His main interest were the kaolin deposits of Yexthó, located one km to the west of the geothermal manifestations. By the middle of the century, the area was already explored for geothermal energy, which resulted in the first geothermal power plant in all America, operating between 1959 and 1972 with a nominal capacity of 3.5 MW. The thermal manifestations of Pathé are located at the junction of two regional normal fault systems, striking N-S and E-W, and are hosted by a volcanic unit (tuff and lava) of basic to intermediate composition and Upper Miocene age. Surficial hydrothermal alteration is conspicuous and largely controlled by faults of these two systems. Associated with the N-S faults is a calcite-gypsum alteration assemblage, indicating oxidized, alkaline sulfate-rich hydrothermal fluids. On the other hand, linked to the later E-W faults are the kaolin deposits; they are the product of an advanced argillic alteration that is characteristic of a steam-heated environment and indicates acidic conditions (pH: 2 to 3) and temperatures around 100 °C. Because of its unambiguous relation to faults and the absence of recent (Quaternary) volcanism, Pathé is likely to be a fault-controlled geothermal system (non-magmatic, extensional domain type). The successive alteration events suggest that the hydrothermal activity is long-lived and dates back to before the Pliocene.doi: https://doi.org/10.22201/igeof.00167169p.2021.60.3.2130

773.1.#.t: Geofísica Internacional; Vol. 60 Núm. 3: Julio 1, 2021; 258-279

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: 258-279

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

doi: https://doi.org/10.22201/igeof.00167169p.2021.60.3.2130

handle: 00bd61e8396ba56b

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

856.#.0.q: application/pdf

file_creation_date: 2022-04-10 21:24:26.0

file_modification_date: 2022-04-10 21:24:26.0

file_creator: Carles Canet

file_name: d3e6027e4d278e858c73ee80b5ba03644d8e597cf4c29ad4643f658f5b6b61cc.pdf

file_pages_number: 22

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245.1.0.b: Apunte geológico y revisión histórica de la zona geotérmica de Pathé, Hidalgo

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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