What can seismic noise tell us about the Alpine reactivation of the Iberian Massif? An example in the Iberian Central System

<p>The Iberian Central System, formed after the Alpine reactivation of the Variscan Iberian Massif, features maximum altitudes of 2500 m. It is surrounded by two foreland basins with contrasting elevation: the Duero Basin to the north, located at 750–800 m, and the Tajo Basin to the south, lyi...

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Bibliographic Details
Main Authors: J. Andrés, P. Ayarza, M. Schimmel, I. Palomeras, M. Ruiz, R. Carbonell
Format: Article
Language:English
Published: Copernicus Publications 2020-12-01
Series:Solid Earth
Online Access:https://se.copernicus.org/articles/11/2499/2020/se-11-2499-2020.pdf