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Geochemical and petrological insights into the tectonic origin of the Transmexican Volcanic Belt
Abstract The Transmexican Volcanic Belt (TMVB) is the magmatic expression of one of the
most complex convergent margins on the planet, and as such constitutes a prime location for …
most complex convergent margins on the planet, and as such constitutes a prime location for …
Petrogénesis ígnea de la faja volcánica transmexicana
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 …
Igneous petrogenesis of the Trans-Mexican volcanic belt
The magmatic diversity of the Trans-Mexican Volcanic Belt is directly or indirectly controlled
by two independent oceanic plates with differing geophysical and compositional …
by two independent oceanic plates with differing geophysical and compositional …
Variation of Cenozoic extension and volcanism across the southern Sierra Madre Occidental volcanic province, Mexico
The middle to late Cenozoic tectonic-magmatic evolution of the Sierra Madre Occidental
volcanic province south of the Tropic of Cancer is summarized and analyzed for the first …
volcanic province south of the Tropic of Cancer is summarized and analyzed for the first …
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 …
Effects of prolonged flat subduction on the Miocene magmatic record of the central Trans-Mexican Volcanic Belt
Temporal changes in the chemical compositions of middle to late Miocene rocks from the
central Trans-Mexican Volcanic Belt elucidate how prolonged flat subduction influences arc …
central Trans-Mexican Volcanic Belt elucidate how prolonged flat subduction influences arc …
Alkalic (ocean-island basalt type) and calc-alkalic volcanism in the Mexican volcanic belt: a case for plume-related magmatism and propagating rifting at an active …
The Mexican volcanic belt has been traditionally regarded as a classic case of subduction-
related calc-alkalic volcanism. However, a series of geologic, geophysical, and petrological …
related calc-alkalic volcanism. However, a series of geologic, geophysical, and petrological …
Temporal control of subduction magmatism in the eastern Trans‐Mexican Volcanic Belt: Mantle sources, slab contributions, and crustal contamination
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 …
Uplift and subduction erosion in southwestern Mexico since the Oligocene: pluton geobarometry constraints
DJ Morán-Zenteno, P Corona-Chavez… - Earth and Planetary …, 1996 - Elsevier
Details of the late Oligocene to Middle Miocene uplift and tectonic erosion episodes of the
southwestern continental margin of Mexico can be inferred using Altot geobarometry of …
southwestern continental margin of Mexico can be inferred using Altot geobarometry of …
Bouguer gravity anomalies and regional crustal structure in central Mexico
J Urrutia-Fucugauchi, JH Flores-Ruiz - International Geology …, 1996 - Taylor & Francis
Analysis of the Bouguer gravity anomalies for central Mexico, between 18° and 21° N and
96° and 106° W, is used to document the regional crustal structure beneath the active …
96° and 106° W, is used to document the regional crustal structure beneath the active …