The basic triggering mechanism underlying induced seismicity traces back to the mid‐1960s
that relied on the process of pore‐fluid pressure diffusion. The last decade has experienced …

Continental-Scale Groundwater Flow and Geologic Processes ADS Classic is now deprecated.
It will be completely retired in October 2019. This page will automatically redirect to the new …

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

Abstract The Sand Hill fault is a steeply dipping, large-displacement normal fault that cuts
poorly lithified Tertiary sediments of the Albuquerque basin, New Mexico, United States. The …

In the Athabasca Basin Proterozoic sandstones unconformably overlie Archean and
Aphebian rocks. Multiple fluid events, involving isotopically-and chemically-distinct fluids …

The Altamont oil field in the deep Uinta basin is known to have reservoir fluid pressures that
approach lithostatic. One explanation for this high pore-fluid pressure is the generation of oil …

Late diagenetic dolomitization of the Lower Ordovician, Upper Knox Group in the southern
Appalachian basin was closely associated with widespread secondary porosity …

Faults in high porosity, Lower Permian sandstones from north-west England and south-west
Scotland occur as millimetre-wide bands of cataclastic deformation, across which shear …

Tunneling in urban areas demands an accurate characterization of the shallow subsurface
to minimize risks during excavation. Unexpected high water inflows constitute a major …

The challenge of this study was to create a 3D geological and structural model of the
Kasserine Aquifer System (KAS) in central Tunisia and its natural extension into north-east …