Two-Dimensional Geothermal Model of the Peruvian Andes above the Nazca Ridge Subduction

Two-Dimensional Geothermal Model of the Peruvian Andes above the Nazca Ridge Subduction

The aseismic Nazca Ridge produces localized flat-slab subduction beneath the South American margin at latitudes 10° to 15° S. The geological evolution and the spatio-temporal pattern of deformation of the upper plate have been strongly influenced by the presence of the flat slab. In this study, we i...

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Bibliographic Details
Main Authors:	Sara Ciattoni, Stefano Mazzoli, Antonella Megna, Matteo Basilici, Stefano Santini
Format:	Article
Language:	English
Published:	MDPI AG 2023-11-01
Series:	Energies
Subjects:	subduction zones slab geometry thermal structure heat flow isotherms
Online Access:	https://www.mdpi.com/1996-1073/16/23/7697

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