Denudation history and palaeogeography of the Pyrenees and their peripheral basins: an 84-million-year geomorphological perspective

M Calvet, Y Gunnell, B Laumonier - Earth-Science Reviews, 2021 - Elsevier
This review provides a synthesis of the evolution of the Pyrenees since~ 84 Ma and is
uniquely focused on analysing jointly and comparatively its peripheral pro-foreland, retro …

Active Tectonics of the Pyrenees: A review.

P Lacan, M Ortuño Candela - Journal Of Iberian Geology, 2012, vol …, 2012 - diposit.ub.edu
The Pyrenees have experienced at least seven earthquakes with magnitude M> 5 in the last
400 years. During the last decades, several seismotectonic, neotectonic and …

[PDF][PDF] The Pyrenean orogen: pre-, syn-, and post-collisional evolution

J Vergés, M Fernàndez, A Martìnez - Journal of the Virtual …, 2002 - academia.edu
The Pyrenean Mountains represent the westernmost end of the long Alpine-Himalayan
collisional system. The excellent preservation of foreland basin deposits in conjunction with …

The recent (upper Miocene to Quaternary) and present tectonic stress distributions in the Iberian Peninsula

M Herraiz, G De Vicente, R Lindo‐Ñaupari, J Giner… - …, 2000 - Wiley Online Library
A general synthesis of the recent and present stress situation and evolution in the Iberian
Peninsula was obtained from microstructural and seismological analysis. The stress …

Inversion of moment tensor focal mechanisms for active stresses around the microcontinent Iberia: Tectonic implications

G De Vicente, S Cloetingh, A Muñoz‐Martín, A Olaiz… - …, 2008 - Wiley Online Library
The Iberian microcontinent and its connected oceanic crust are affected by deformations
related to the Eurasian‐African plate boundary. Active stress inversions from populations of …

Test of the frictional reactivation theory for faults and validity of fault-slip analysis

RJ Lisle, DC Srivastava - Geology, 2004 - pubs.geoscienceworld.org
The notion that slip on faults is controlled by the balance between resolved shear stress and
the magnitude of frictional resistance is examined in the light of the published orientations of …

Topographic and faults control of hydrothermal circulation along dormant faults in an orogen

A Taillefer, L Guillou‐Frottier, R Soliva… - Geochemistry …, 2018 - Wiley Online Library
Hydrothermal systems involving dormant faults within orogenic belts are rarely targeted for
geothermal exploration, partly because of the complexity of the 3‐D topography, the …

TOPO-EUROPE: The geoscience of coupled deep Earth-surface processes

S Cloetingh, PA Ziegler, PJF Bogaard… - Global and Planetary …, 2007 - Elsevier
TOPO-EUROPE addresses the 4-D topographic evolution of the orogens and intra-plate
regions of Europe through a multidisciplinary approach linking geology, geophysics …

Fault‐Related Controls on Upward Hydrothermal Flow: An Integrated Geological Study of the Têt Fault System, Eastern Pyrénées (France)

A Taillefer, R Soliva, L Guillou-Frottier, E Le Goff… - …, 2017 - Wiley Online Library
The way faults control upward fluid flow in nonmagmatic hydrothermal systems in
extensional context is still unclear. In the Eastern Pyrénées, an alignment of twenty‐nine hot …

Present-day deformation of the Pyrenees revealed by GPS surveying and earthquake focal mechanisms until 2011

A Rigo, P Vernant, KL Feigl, X Goula… - Geophysical Journal …, 2015 - academic.oup.com
The Pyrenean mountain range is a slowly deforming belt with continuous and moderate
seismic activity. To quantify its deformation field, we present the velocity field estimated from …