The anomalous enrichment of clay minerals in fault zones is considered a key factor
affecting the seismic behavior of faults, fault permeability, and mineralization. This process …

Magmatic arcs may play a major role in the initiation, behavior, and abandonment of intra‐
arc strike‐slip systems. Here we present zircon U‐Pb and (U‐Th)/He geochronology …

We describe the structural features and mineralogical and geochemical compositions of the
fault rocks recovered from boreholes at the Golden River site on the Yingxiu–Beichuan fault …

This study combines multiscale analyses of geological, fault, fracture, and stable isotope
data to investigate strike-slip deformation and channeling of hydrothermal fluids along the …

Understanding fault zone permeability and its spatial distribution allows the assessment of
fluid-migration leading to precipitation of hydrothermal minerals. This work is aimed at …

Abstract The Alpine Fault has a< 50 m wide geochemically distinct hanging-wall alteration
zone. Using a combination of petrological and cathodoluminescence (CL) microscopy …

Abundant geothermal springs occur along the Moxi fault located in western Sichuan
Province (the eastern edge of the Qinghai-Tibet plateau), highlighted by geothermal water …

Exhumed faults in granitoids along the Lanterman Fault-Rennick Graben Fault system
(northern Victoria Land, Antarctica) show superposed ductile to brittle deformation and …

The Paposo fault zone is a major brittle-ductile strand of the Atacama fault system (AFS),
which records sinistral shear associated with Cretaceous oblique subduction beneath …

Tectonic pseudotachylytes are thought to be unique to certain water‐deficient seismogenic
environments and their presence is considered to be rare in the geological record. Here, we …