Denudation history and palaeogeography of the Pyrenees and their peripheral basins: an 84-million-year geomorphological perspective
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 …
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 …
400 years. During the last decades, several seismotectonic, neotectonic and …
The recent (upper Miocene to Quaternary) and present tectonic stress distributions in the Iberian Peninsula
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 …
Peninsula was obtained from microstructural and seismological analysis. The stress …
Topographic and faults control of hydrothermal circulation along dormant faults in an orogen
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 …
geothermal exploration, partly because of the complexity of the 3‐D topography, the …
Fault‐Related Controls on Upward Hydrothermal Flow: An Integrated Geological Study of the Têt Fault System, Eastern Pyrénées (France)
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 …
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
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 …
seismic activity. To quantify its deformation field, we present the velocity field estimated from …
A new synthesis of Pyrenean seismicity and its tectonic implications
A Souriau, H Pauchet - Tectonophysics, 1998 - Elsevier
The Pyrenean range, which results from the convergence of the Iberian and Eurasian plates
along the North Pyrenean fault, exhibits a permanent seismic activity with moderate …
along the North Pyrenean fault, exhibits a permanent seismic activity with moderate …
New geomorphic evidence for anticlinal growth driven by blind-thrust faulting along the northern Marche coastal belt (central Italy)
Abstract The Northern Marche coastal belt is characterised by a series of NW-SE trending,
NE verging folds forming the easternmost edge of the Apennines thrust front. Several …
NE verging folds forming the easternmost edge of the Apennines thrust front. Several …
Present and recent stress regime in the eastern part of the Pyrenees
X Goula, C Olivera, J Fleta, B Grellet, R Lindo… - Tectonophysics, 1999 - Elsevier
Earthquake focal mechanisms and microtectonic analysis of fault striation are presented in
order to study the regional state of stress in the eastern part of the Pyrenees. The inversion …
order to study the regional state of stress in the eastern part of the Pyrenees. The inversion …
Large‐scale rock slope failures in the eastern pyrenees: identifying a sparse but significant population in paraglacial and parafluvial contexts
D Jarman, M Calvet, J Corominas… - … Annaler: Series A …, 2014 - Taylor & Francis
This first overview of large‐scale rock slope failure (RSF) in the yrenees addresses the
eastern third of the range. Around 30 principal RSFs greater than 0.25 km2 and 20 lesser or …
eastern third of the range. Around 30 principal RSFs greater than 0.25 km2 and 20 lesser or …