Deformation along faults in the shallow crust (< 1 km) introduces permeability heterogeneity
and anisotropy, which has an important impact on processes such as regional groundwater …

Heat carried by ground water serves as a tracer to identify surface water infiltration, flow
through fractures, and flow patterns in ground water basins. Temperature measurements …

In semiarid climates, a significant component of recharge to basin aquifers occurs along the
mountain front. Traditionally called" mountain-front recharge"(MFR), this process has been …

We argue that the observed conduit‐barrier behavior of fault zones in siliciclastic
sedimentary aquifer systems can be understood by considering a strongly anisotropic …

Groundwaters of the southern Colorado Plateau–Arizona Transition Zone region are a
heterogeneous mixture of chemically diverse waters including meteoric (epigenic) fluids …

Des failles recoupant des sédiments non consolidés du système du rift de la vallée de la
Roer (Pays-Bas) forment en général de fortes barrières vis-à-vis des écoulements …

Hydrogeochemical investigation was carried out in the Western Doon valley, to understand
the geochemistry of the groundwater and to assess the overall physic-chemical …

Based on various lines of geologic, geomorphic, topographic, geophysical, spectral, and
elemental evidence, we conclude that hydrothermal environments have certainly existed on …

In the present paper it is shown how profiles consisting of closely spaced (≤ 10 m)
temperature measurements at shallow depth, obtained at several instances during one …

This study aims to investigate groundwater recharge and flow patterns in tectonically active
rift systems, exemplified by a case study in the Main Ethiopian Rift. The chosen approach …