Why has the Nazca plate slowed since the Neogene?

The classic example of the not-well-understood rapid change of tectonic plate motion is the increase and then decrease of the convergence rate between the Nazca and South America plates during the past 25-20 m.y. that coincided with the growth of the Andes Mountains. Currently, the decrease in conve...

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Detalles Bibliográficos
Autor principal:	Quinteros, Javier
Publicado:	2013
Materias:	Convergence rates Lower mantle Natural consequences Nazca plate Neo genes Oblique subduction Seismic tomographic images South America Tectonic plates Thermo-mechanical Transition zones View-based Geology Tomography Neogene plate motion seismic tomography subduction zone transition zone Andes
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00917613_v41_n1_p31_Quinteros http://hdl.handle.net/20.500.12110/paper_00917613_v41_n1_p31_Quinteros
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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