dor_id: 42565

506.#.#.a: Público

590.#.#.d: Cada artículo es evaluado mediante una revisión ciega única. Los revisores son externos nacionales e internacionales.

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT), Sistema Regional de Información en Línea para Revistas Científicas de América Latina, el Caribe, España y Portugal (Latindex), Scientific Electronic Library Online (SciELO), SCOPUS, Web Of Science (WoS)

561.#.#.u: http://www.geofisica.unam.mx/

650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: info:eu-repo/semantics/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: http://www.revistas.unam.mx/front/

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, UNAM

850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/604/587

100.1.#.a: Macías, José Luís; Capaccioni, Bruno; Conticelli, Sandro; Martini, Marino; Rodríguez, Sergio

524.#.#.a: Macías, José Luís, et al. (1993). Volatile elements in alkaline and calc-alkaline rocks from the Colima graben, Mexico: Constrains on their genesis and evolution. Geofísica Internacional; Vol. 32 No. 4, 1993. Recuperado de https://repositorio.unam.mx/contenidos/42565

245.1.0.a: Volatile elements in alkaline and calc-alkaline rocks from the Colima graben, Mexico: Constrains on their genesis and evolution

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1993

264.#.1.c: 2013-06-10

653.#.#.a: Volatile elements; fluorine; Colima graben; Mexico.; Elementos volátiles; fluor; Colima graben; México.

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-ND 4.0 Internacional, https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode.es, fecha de asignación de la licencia 2013-06-10, para un uso diferente consultar al responsable jurídico del repositorio por medio de revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/604

001.#.#.#: oai:ojs.ojs.geofisica.unam.mx:article/604

041.#.7.h: spa

520.3.#.a: Based on major element chemical composition, three groups of rocks having different parental magmas can be recognized in Colima graben region. The most mafic rocks belong to the alkaline group, which display the highest incompatible and compatible element contents among the rocks studied. The second group, the calc-alkaline volcanic have the largest compositional range among the rocks studied due probably to low pressure evolutionary processes. A third group straddles the subalkaline-alkaline field boundary, and has K2O abundances intermediate between alkaline and calc-alkaline volcanic. Primitive rocks were neither found in calc-alkaline nor in high potassium calc-alkaline rocks. All the rocks studied have similar hydromagmaphile patterns with high LILE/HFSE values. Halongens (F and Cl), S and C analyses have been performed on the majority of the samples from the three groups of rocks of the Colima region. All the most primitive rocks of the three groups are characterized by comparable low abundances of C and S. Cl is initially relatively low, but tends to increase with the degree of evolution in calc-alkaline and high potassium calc-alkaline rocks, although some samples seem to have lost halogens by exsolution in a shallow level magnetic reservoir. The fluorine and potassium abundances seem to indicate phlogopite as one of the mineral phases in the Colima sub-arc mantle. A mica-bearing mantle source affected by different degrees of partial melting can be hypothesized for the genesis of alkaline and calc-alkaline parental magma. Nevertheless, this has to be still considered as a working hypothesis and further mineralogical, geochemical and petrological studies must be performed to better constrain the role of evolution in the genesis of studied rocks.

773.1.#.t: Geofísica Internacional; Vol. 32 No. 4 (1993)

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

046.#.#.j: 2020-10-20 00:00:00.000000

022.#.#.a: 0016-7169

310.#.#.a: Trimestral

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

758.#.#.1: http://revistagi.geofisica.unam.mx/index.php/RGI

handle: 20ff5a3ebd65eb9f

harvesting_date: 2020-09-23 00:00:00.0

856.#.0.q: application/pdf

file_modification_date: 2014-12-23 15:10:37.0

last_modified: 2020-10-21 00:00:00

license_url: https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode.es

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