The dynamic history of the Trans-Mexican Volcanic Belt and the Mexico subduction zone
The Trans-Mexican Volcanic Belt (TMVB) is a 1000km long Neogene continental arc
showing a large variation in composition and volcanic style, and an intra-arc extensional …
showing a large variation in composition and volcanic style, and an intra-arc extensional …
'Large Igneous Provinces (LIPs)': Definition, recommended terminology, and a hierarchical classification
HC Sheth - Earth-Science Reviews, 2007 - Elsevier
This article is an appeal for the adoption of a correct and appropriate terminology with
respect to the so-called Large Igneous Provinces (LIPs). The term LIP has been widely …
respect to the so-called Large Igneous Provinces (LIPs). The term LIP has been widely …
Petrogénesis ígnea de la faja volcánica transmexicana
A Gómez-Tuena, MT Orozco-Esquivel… - Boletín de la Sociedad …, 2005 - scielo.org.mx
La extraordinaria diversidad magmática de la Faja Volcánica Transmexicana está
controlada (directa o indirectamente) por dos placas oceánicas independientes cuyos …
controlada (directa o indirectamente) por dos placas oceánicas independientes cuyos …
Provenance of sands from cazones, acapulco, and bahía kino beaches, México
JS Armstrong-Altrin - Revista mexicana de ciencias geológicas, 2009 - scielo.org.mx
Petrographic, major, trace, and rare-earth element geochemistry of sands from three
beaches of México (Cazones, Acapulco, and Bahía Kino) were studied to determine their …
beaches of México (Cazones, Acapulco, and Bahía Kino) were studied to determine their …
Geología e historia eruptiva de algunos de los grandes volcanes activos de México
JL Macías - Boletín de la Sociedad Geológica Mexicana, 2005 - scielo.org.mx
La mayor parte de los grandes volcanes de nuestro país se encuentran ubicados en la parte
frontal de la Faja Volcánica Transmexicana y en otras zonas volcánicas aisladas. En este …
frontal de la Faja Volcánica Transmexicana y en otras zonas volcánicas aisladas. En este …
Discriminating four tectonic settings: Five new geochemical diagrams for basic and ultrabasic volcanic rocks based on log—ratio transformation of major-element data
We present five new discriminant function diagrams based on an extensive database
representative of basic and ultrabasic rocks from four tectonic settings of island arc …
representative of basic and ultrabasic rocks from four tectonic settings of island arc …
Temporal control of subduction magmatism in the eastern Trans‐Mexican Volcanic Belt: Mantle sources, slab contributions, and crustal contamination
A Gómez‐Tuena, AB LaGatta… - Geochemistry …, 2003 - Wiley Online Library
The magmatic record of the easternmost part of the Trans‐Mexican Volcanic Belt elucidates
how temporal changes in subduction parameters influence convergent margin volcanism. In …
how temporal changes in subduction parameters influence convergent margin volcanism. In …
[PDF][PDF] Volcanic stratigraphy and geological evolution of the Apan region, east-central sector of the Trans-Mexican Volcanic Belt
La región de Apan está situada entre los sectores este y central del Cinturón Volcánico
Transmexicano (CVTM), su registro geológico muestra una interacción intermitente entre …
Transmexicano (CVTM), su registro geológico muestra una interacción intermitente entre …
Geochemistry, Sr–Nd isotope composition, and tectonic setting of Holocene Pelado, Guespalapa and Chichinautzin scoria cones, south of Mexico City
Holocene Pelado, Guespalapa and Chichinautzin monogenetic scoria cones and
associated lava flows located within the Sierra del Chichinautzin Volcanic Field (SCVF) at …
associated lava flows located within the Sierra del Chichinautzin Volcanic Field (SCVF) at …
[PDF][PDF] From Deccan to Réunion: no trace of a mantle plume
HC Sheth - Special Papers-Geological Society of America, 2005 - chip.chagos-trust.org
The widely accepted mantle plume model postulates that (1) the currently volcanically active
Réunion Island in the Indian Ocean is fed by the narrow “tail” of a mantle plume that rises …
Réunion Island in the Indian Ocean is fed by the narrow “tail” of a mantle plume that rises …