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 …
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 …
[图书][B] Introduction to volcanic seismology
VM Zobin - 2011 - books.google.com
Volcanic seismology represents the main, and often the only, tool to forecast volcanic
eruptions and to monitor the eruption process. This book describes the main types of seismic …
eruptions and to monitor the eruption process. This book describes the main types of seismic …
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 …
Debris avalanches and debris flows transformed from collapses in the Trans-Mexican Volcanic Belt, Mexico–behavior, and implications for hazard assessment
Volcanoes of the Trans-Mexican Volcanic Belt (TMVB) have yielded numerous sector and
flank collapses during Pleistocene and Holocene times. Sector collapses associated with …
flank collapses during Pleistocene and Holocene times. Sector collapses associated with …
The cohesive Naranjo debris-flow deposit (10 km3):: A dam breakout flow derived from the Pleistocene debris-avalanche deposit of Nevado de Colima Volcano …
Mass movement processes on volcanic terrains such as landslides and debris avalanches
can cause the obstruction of main drainages producing the formation of temporary dams. A …
can cause the obstruction of main drainages producing the formation of temporary dams. A …
Experimental constraints on volatile abundances in arc magmas and their implications for degassing processes
B Scaillet, M Pichavant - 2003 - pubs.geoscienceworld.org
Recent phase equilibrium studies, combined with analytical and petrological data, provide
rigorous constraints on the pre-eruptive PTf H 2 0-fO 2-fS 2-fCO 2 conditions of silicic to …
rigorous constraints on the pre-eruptive PTf H 2 0-fO 2-fS 2-fCO 2 conditions of silicic to …
Overview of the 1997–2000 activity of Volcán de Colima, Mexico
This overview of the 1997–2000 activity of Volcán de Colima is designed to serve as an
introduction to the Special Issue and a summary of the detailed studies that follow. New …
introduction to the Special Issue and a summary of the detailed studies that follow. New …
Response of a landscape to tectonics using channel steepness indices (ksn) and OSL: A case of study from the Jalisco Block, Western Mexico
Rapid tectonic uplift is known to increase river incision rates and to trigger the propagation of
knickpoints along a river profile, augmenting local relief. Thus, the topography of …
knickpoints along a river profile, augmenting local relief. Thus, the topography of …
Structural architecture of the Colima volcanic complex
The Colima Volcanic Complex (CVC) is currently the most active Mexican volcano and is
located in the western sector of the Trans–Mexican Volcanic Belt, inside the active Colima …
located in the western sector of the Trans–Mexican Volcanic Belt, inside the active Colima …