Título
Petrogenetic and tectonic implications of major and trace element and radiogenic isotope geochemistry of Pliocene to Holocene rocks from the Tacaná Volcanic Complex and Chiapanecan Volcanic Belt, southern Mexico
11627/516411627/5164
Autor
Verma Jaiswal, Surendra Pal
Verma, Sanjeet Kumar
Resumen
"New major and trace element, and Sr, Nd and Pb isotope data for samples from the Volcán Tacaná, along with the published data from the Tacaná Volcanic Complex (TVC) and Chiapanecan Volcanic Belt (CVB), were used to better constrain the petrogenesis of the Pliocene to Holocene volcanism in southwestern Mexico. The TVC volcanic rocks sampled in this study were andesite, whereas the literature samples included, besides andesites, one subalkali basalt and a few dacites. The CVB housing the prominent El Chichón volcano, on the other hand, showed more alkalic magmatic products (trachyandesite and basaltic trachyandesite) but also included a few basalts and dacites. The enclaves and lithic fragments sampled from both TVC and CVB showed wide SiO2 compositions similar to the volcanic products. The CVB rocks are more enriched in REE, LILE, and HFSE than the TVC. The combined data of volcanic rocks were evaluated through conventional multi-element diagrams as well as subduction- or crust-sensitive parameters. Although the TVC constitutes the northern end of the Central American Volcanic Arc (CAVA), some chemical differences were documented between them such as the TVC rocks have higher LILE, REE, HFSE, and combined ratio parameters. More importantly, the CVB seems to be significantly different from both TVC and CAVA as well as from other continental arcs such as higher LILE, REE, HFSE, and distinct isotopic signature, which may indicate that the origin of the CVB volcanism represents a direct action of the abundant strike-slip faults and extensional system prevalent in this area. Finally, the relationship of basic and evolved rocks from the CVB, especially on isotope-isotope diagrams, also suggests that the lower crust may have contributed to evolved magmas during the ascent of basic magmas through the crust."
Fecha de publicación
2018Tipo de publicación
articleDOI
https://doi.org/10.1016/j.lithos.2018.05.016Área de conocimiento
GEOQUÍMICAColecciones
Editor
ElsevierPalabras clave
Central American Volcanic ArcTacaná Volcanic Complex
Geochemometrics
Southern Mexico
Chiapanecan Volcanic Arc
Subduction
Strike-slip faulting
Extension
Citar Como
Surendra P. Verma, Sanjeet K. Verma, Petrogenetic and tectonic implications of major and trace element and radiogenic isotope geochemistry of Pliocene to Holocene rocks from the Tacaná Volcanic Complex and Chiapanecan Volcanic Belt, southern Mexico, Lithos, Volumes 312–313, 2018, Pages 274-289.Archivos
Metadatos
Mostrar el registro completo del ítem
Excepto si se señala otra cosa, la licencia del ítem se describe como Attribution-NonCommercial-NoDerivatives 4.0 Internacional
Ítems relacionados
Mostrando ítems relacionados por Título, autor o materia.
-
The Ahualulco Volcanic Complex: Geochemistry and temporal evolution of Oligocene felsic volcanism, in the east of the Mesa Central, San Luis Potosí, Mexico [El complejo volcánico de Ahualulco: geoquímica y evolución temporal del vulcanismo félsico del Oligoceno, en el oriente de la Mesa Central, San Luis Potosí, México]
Latorre Correa, Carolina Isabel; Dávila Harris, Pablo; Aguillón Robles, Alfredo; Tristán González, Margarito (Instituto de Geociencias, UNAM, 2023)The Ahualulco Volcanic Complex (AVC), in the southern region of the Mesa Central of Mexico, consists of a set of Cenozoic volcanic rocks, which includes andesites. The AVC was emplaced in the middle Eocene, followed by ... -
The regional influence of volcanic emissions from Popocateptl, Mexico
Pyle, David M; A Mather, Tamsin (2005) -
Detection of aeromagnetic anomaly change associated with volcanic activity
Nakatsuka, Tadashi; Utsugi, Mitsuru; Okuma, Shigeo; Tanaka, Yoshikazu; Hashimoto, Takeshi (2009)