The dynamic history of the Trans-Mexican Volcanic Belt and the Mexico subduction zone

L Ferrari, T Orozco-Esquivel, V Manea, M Manea - Tectonophysics, 2012‏ - Elsevier
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 …

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 …

Igneous petrogenesis of the Trans-Mexican volcanic belt

A Gómez-Tuena, MT Orozco-Esquivel, L Ferrari - 2007‏ - pubs.geoscienceworld.org
The magmatic diversity of the Trans-Mexican Volcanic Belt is directly or indirectly controlled
by two independent oceanic plates with differing geophysical and compositional …

Quaternary intra-arc extension in the central Trans-Mexican volcanic belt

M Suter, ML Martínez… - … Society of America …, 2001‏ - pubs.geoscienceworld.org
Abstract The Trans-Mexican volcanic belt is an active volcanic arc related to subduction
along the Middle America trench and characterized by shallow seismicity and synvolcanic to …

The control of preexisting faults on the distribution, morphology, and volume of monogenetic volcanism in the Michoacán-Guanajuato Volcanic Field

MG Gómez-Vasconcelos, JL Macías… - …, 2020‏ - pubs.geoscienceworld.org
Interactions between volcanic and tectonic processes affect the distribution, morphology,
and volume of eruptive products in space and time. The Queréndaro area in the eastern …

[HTML][HTML] Paleoseismology of the southwestern Morelia-Acambay fault system, central Mexico

VH Garduño-Monroy, R Pérez-López… - Geofísica …, 2009‏ - scielo.org.mx
El sistema de fallas Morelia–Acambay (MAFS) consiste en una serie de fallas normales de
dirección E–W y NE–SW que cortan la parte central del Cinturón Volcánico Transmexicano …

Rapid evolution of subduction‐related continental intraarc rifts: The Taupo Rift, New Zealand

P Villamor, KR Berryman, SM Ellis, G Schreurs… - …, 2017‏ - Wiley Online Library
The evolution of the continental intraarc Taupo Rift in the North Island, New Zealand, is
rapid, significantly faster than comparative intracontinental rifts such as the African Rifts …

Palaeoenvironmental significance of diatom and vertebrate fossils from Late Cenozoic tectonic basins in west-central México: A review

I Israde-Alcántara, WE Miller, VH Garduño-Monroy… - Quaternary …, 2010‏ - Elsevier
Pronounced lacustrine sedimentation developed in west-central México during the late
Miocene, between approximately 11 and 7 Ma. This was in response to tectonic extension …

Late Pleistocene Alberca de Guadalupe maar volcano (Zacapu basin, Michoacán): Stratigraphy, tectonic setting, and paleo-hydrogeological environment

P Kshirsagar, C Siebe, MN Guilbaud, S Salinas… - Journal of Volcanology …, 2015‏ - Elsevier
Abstract The Late Pleistocene (~ 21,000 yr BP) Alberca de Guadalupe maar is one of the
few phreatomagmatic volcanoes occurring within the scoria-cone dominated Plio …

The eruptive history of the Pátzcuaro Lake area in the Michoacán Guanajuato Volcanic Field, central México: Field map**, C-14 and 40Ar/39Ar geochronology

S Osorio-Ocampo, JL Macías, A Pola… - Journal of Volcanology …, 2018‏ - Elsevier
Monogenetic volcanic fields occur in many tectonic settings representing an unpredictable
and uncertain volcanic hazard. The Pátzcuaro Lake is located in the central part of the …