Although the widths of fault damage zones commonly show a positive correlation with
displacements, these relationships also show a somewhat scattered distribution. We believe …

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 …

It is increasingly apparent that faults are typically not discrete planes but zones of deformed
rock with a complex internal structure and three-dimensional geometry. In the last decade …

This study addresses the interplay between strain/stress fields and paleo-fluid migration in
the Southern Andean Volcanic Zone (SVZ). The SVZ coexists with the margin-parallel …

Earthquake source mechanisms and spectra can provide important clues to aid in
discriminating between natural and induced events. In this study, we calculate moment …

It is widely recognized that fluid injection can trigger aseismic fault slip. However, the
processes by which the fluid‐rock interactions facilitate or inhibit slip are poorly understood …

The strike-slip fault zones (SSFZs) of the central Tarim Basin have great potential for
hydrocarbon exploration and development. They can both serve as hydrocarbon migration …

Growing macroscale fold structures are one of the most dynamic and complex systems in
geology, where during fold growth pore fluid pressure, fluid temperature, and fluid …

Although fluid–rock chemical interactions are common natural phenomena associated with
ore-forming systems in the crust of the Earth, they may find applications in the utilization of …

Numerical experiments were carried out to investigate the fluid flow in typical Proterozoic
basins that host unconformity-related uranium deposits. We have constructed a simplified …