RT Journal Article
T1 Reactivación intraplaca de un relieve apalachiano: Las Sierras de Guadalupe y Montánchez
A1 Álvarez, J.
A1 Muñoz Martín, Alfonso
A1 Vicente Muñoz, Gerardo De
A1 Vegas Martínez, Ramón
AB In this work, we reconcile structural data analysis with géomorphologie observations to better constrain the morphotectonic evolution of the Guadalupe and Montánchez intraplate ranges located in western central Iberia. Fault slip data analysis and geological mapping suggest a global episode of uplift and northwest tilting during Pliocene times. The Hercynian basement was then uplifted by a NW verging thrust developing Plio-Quaternary syntectonic alluvial fans "Raña deposits". The present-day landscape of these ranges should be interpreted as a result of the interaction of (neo) tectonic forcing and longitudinal fluvial erosion.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2004
FD 2004
LK https://hdl.handle.net/20.500.14352/52554
UL https://hdl.handle.net/20.500.14352/52554
LA spa
DS Docta Complutense
RD 8 ago 2024