Thermal and geodynamic contributions to the elevation of the Altiplano-Puna plateau

The most remarkable feature of the Central Andes is the Altiplano-Puna plateau. This plateau is characterized by 3.5. km average elevation, approximately 70. km crustal thickness and very high heat flow. The upper mantle structure changes along strike below the plateau. The upper mantle below the Pu...

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Detalles Bibliográficos
Autores principales:	Prezzi, C., Iglesia Llanos, M.P., Götze, H.-J., Schmidt, S.
Formato:	JOUR
Materias:	Altiplano-Puna Geodynamic topography Thermal isostasy Topography Geodesy Geodynamics Thermal expansion Crustal thickness Geodynamic process Regional variation Thermal component Thermal contributions Upper mantle structure Structural geology crustal thickness elevation geodynamics isostasy lithosphere mantle structure plate tectonics plateau topographic effect upper mantle Altiplano Puna
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00319201_v237_n_p51_Prezzi
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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