Springs sustain groundwater-dependent ecosystems and provide freshwater for human use.
Springs often occur because faults modify groundwater flow pathways leading to discharge …

We propose a review to discuss the large number of studies dealing with the fluid history in
extensional and compressional sedimentary basins that evolved along the Iberian-Eurasian …

A renewed interest in fault damage zones is aimed at better understanding stress
perturbation around faults, earthquake ground motions and fluid flow in the upper crust. In …

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 …

Résumé The potential of high-temperature (> 150 C) geothermal systems in crustal fault
zones (fault cores and hundreds of meters wide networks of interconnected fractures in the …

The present study aims to understand the potential of a new and novel type of geothermal
play system for high temperature and electricity production: crustal fault zones (CFZ) …

Melting at the base of the Antarctic Ice Sheet influences ice dynamics and our ability to
recover ancient climatic records from deep ice cores. Basal melt rates are affected by …

Deep, large faults are well-developed in the Red River Fault Zone in Yunnan in southwest
China. This study uses a classification approach and macro-scale analysis of faults and hot …

In the first kilometers of the subsurface, temperature anomalies due to heat conduction
processes rarely exceed 20–30∘ C. When fault zones are sufficiently permeable, fluid flow …

The Têt fault is a major crustal-scale fault in the eastern Pyrenees (France) along which 29
hot springs emerge, mainly within the footwall damage zone of the fault. In this study,(U …