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 …

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 …

The large (≈ 10000 km2) and local-scale (< 400 km2) geomorphologic, geomorphometric
and field evidence indicates that, from the mid-Miocene onwards, the Atacama Fault System …

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 …

Our study aims at calculating morphometric indices through the recourse to the Digital
Elevation Model (DEM) and its attributes (hydrographic networks, watersheds, and reliefs) …

In this paper we concentrate particularly on the geomorphological indicators left by active
tectonics. In the central foothills of Taiwan, we used topography, drainage pattern and …

Studying hydrothermal systems in basement environments requires knowledge of fault and
fracture network distributions. This study addresses this through multi-scale structural …

L'expression morphologique de la faille de la Têt ressemble à celle d'une faille active. Son
fonctionnement, attesté pour le Pliocène, reste cependant débattu pour le Pléistocène. Un …

Although the seismic activity at the eastern Pyrenees is nowadays moderate and sparse,
with events usually not exceeding magnitudes 4.5, this area has been affected in the past by …

Les systèmes hydrothermaux non-magmatiques en contexte orogénique sont peu étudiés.
Les questions qui demeurent sont: 1) quelles sont les structures efficaces pour l'infiltration …