dor_id: 4132253

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/1372/1374

100.1.#.a: Delgado-argote, L. A.; Casar-aldrete, I.; González-caver, E.; Morales-puente, P.; Girón-garcía, P.

524.#.#.a: Delgado-argote, L. A., et al. (1993). Geologic controls of hydrogen isotope ratios of structural water in serpentinites from San Pedro Limon-Palmar Chico, Tierra Caliente Terrane, Mexico. Geofísica Internacional; Vol. 32 Núm. 3: Julio 1, 1993; 415-427. Recuperado de https://repositorio.unam.mx/contenidos/4132253

245.1.0.a: Geologic controls of hydrogen isotope ratios of structural water in serpentinites from San Pedro Limon-Palmar Chico, Tierra Caliente Terrane, Mexico

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1993

264.#.1.c: 1993-07-01

653.#.#.a: Isotópos de hidrogeno; serpentinita; cretácico; espectroscopía de infrarojo; area de San Pedro; Limón-Palmar Chico; complejo de tierra caliente; Hydrogen isotopes; serpentinite; cretaceous; infrared spectroscopy; San Pedro Limón-Palmar Chicho

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/1372

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1372

041.#.7.h: spa

520.3.#.a: The area of San Pedro Limon-Palmar Chico is geologically located in the Tierra Caliente Complex. The complex is composed of an Albian-Cenomanian volcano sedimentary sequence of island arc type. A series of volcanic edifices is interpreted from the features of volcanic and sedimentary facies. The sedimentary sequences (mainly clastic) were deposited in small basins. structurally controlled by the volcanoes. In San Pedro Limon, a 15 km2 dioritic to peridotitic stock intrudes mainly the sedimentary sequence, whereas small wedges of serpentinites not larger than I km2 are emplaced along N-NW structural trends. The San Pedro Limon stock is interpreted as having been emplaced by a torsion mechanism during a Neogene transpressive disturbance. The stock shows a transitional petrographic variation from hornblende-rich diorites to clinopyroxene-rich peridotites with intermediate hornblende pyroxenite (orthopyroxene<1 0%) and pyroxene hornblendite facies. Nine ultramafic samples. ranging from 10% to 100% serpentinization, were analyzed by infrared spectroscopy. Only low-temperature serpentines such as lizardite and chrysotile were identified. Hydrogen isotopic ratios were determined on structural water from nine serpentinites and one sample of chrysotile. 00 ranges from -85 to -116 per mil. Which unequivocally indicates a meteoric origin. Furthermore, the 00 values decrease with increasing degree of serpentinization.The serpentinization must have occurred at low temperature under kinetic conditions. The main serpentinization phase is associated with a tectonic transpressive regime, IWld occurred simultaneously with the mechanical emplacement. of intrusives which developed local hydrothermal conditions.doi: https://doi.org/10.22201/igeof.00167169p.1993.32.3.519

773.1.#.t: Geofísica Internacional; Vol. 32 Núm. 3: Julio 1, 1993; 415-427

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: 415-427

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

doi: https://doi.org/10.22201/igeof.00167169p.1993.32.3.519

handle: 00e81d1b998f90c6

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

856.#.0.q: application/pdf

file_creation_date: 2008-03-25 16:16:48.0

file_modification_date: 2022-07-28 16:28:49.0

file_creator: L. A. Delgado-Argote

file_name: f61cb4ef91163ebb12a494b10cde1d7e37e7398889e16ee61de425e96e058e2c.pdf

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245.1.0.b: Geologic controls of hydrogen isotope ratios of structural water in serpentinites from San Pedro Limon-Palmar Chico, Tierra Caliente Terrane, 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

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