Normal fault relay structures form at all scales as faults interact or step out of their own plane
during growth, and their successive formation and destruction represent the most efficient …

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 …

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

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

Clay smear is a collection of fault processes and resulting fault structures that form when
normal faults deform layered sedimentary sections. These elusive structures have attracted …

First reported in the 1960s, offshore freshened groundwater (OFG) has now been
documented in most continental margins around the world. In this review we compile a …

Although offshore freshened groundwater (OFG) systems have been documented in
numerous continental margins worldwide, their geometry, controls and emplacement …

Structural complexity along faults (eg, relay zones, fault intersections and jogs) exert strong
controls on fluid flow, yet few attempts have been made to quantify and visualise such …

Significant uncertainties occur through varying methodologies when interpreting faults using
seismic data. These uncertainties are carried through to the interpretation of how faults may …

Monogenetic basaltic volcanism is characterised by a complex array of eruptive behaviours,
reflecting spatial and temporal variability of the magmatic properties (eg composition …