CORDIS Project
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This research examines the relationship between geological features and mantle processes in the Andes. By simulating mantle flow and analyzing geological data, the project aims to understand how these dynamics influence surface topography and basin subsidence.
In the world, there is a relative paucity of studies that correlate surface data with deep Earth processes.
The main objective of this experiment is to introduce a series of observations from geology (basins, thrust belts and plateaus) to constrain mantle flow models and better understand the topographic signal generated by the mantle.
We propose to test an active and natural laboratory:
The Andes.
The study will embrace the Andean history from Miocene to Present, the main orogenic phase of Sout…
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