Gomez-Tuena, Arturo; Orozco-Esquivel, Maria Teresa; Ferrari, Luca (2007): Igneous petrogenesis of the Trans-Mexican volcanic belt. Geological Society of America (GSA), Boulder, CO, United States, In: Alaniz-Alvarez, Susana Alicia (editor), Nieto-Samaniego, Angel Francisco (editor), Geology of Mexico; celebrating the centenary of the Geological Society of Mexico, 422, 129-181, georefid:2007-114031

Abstract:
The magmatic diversity of the Trans-Mexican Volcanic Belt is directly or indirectly controlled by two independent oceanic plates with differing geophysical and compositional parameters; by an extensional tectonic regime that operates with different intensities over the upper plate; by a continental basement with a diversity of ages, thicknesses, and compositions; and by a compositionally heterogeneous mantle wedge that has been modified to various extents by the slab-derived chemical agents. The convergent margin and the magmatic arc have not remained static throughout their geologic histories, but instead have shown significant changes in position, geometry, and composition. For these reasons, the Trans-Mexican Volcanic Belt is the result of one of the most complex convergent margins on the planet, the subject of more than a century of scientific investigations, and at the core of the most notorious debates on Mexican geology.
Coverage:
West: -105.0000 East: -94.0000 North: 22.0000 South: 16.0000
West: NaN East: NaN North: NaN South: NaN
Relations:
Expedition: 66
Site: 66-487
Data access:
Provider: SEDIS Publication Catalogue
Data set link: http://sedis.iodp.org/pub-catalogue/index.php?id=10.1130/2007.2422(05) (c.f. for more detailed metadata)
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