Veins are common features in rocks and extremely useful structures to determine stress,
strain, pressure, temperature, fluid composition and fluid origin during their formation. Here …

The interface between subducting oceanic slabs and the hanging wall is a structurally and
lithologically complex region. Chemically disparate lithologies (sedimentary, mafic and …

Geofluids (2010) 10, 193–205 Abstract The variation of permeability with depth can be
probed indirectly by various means, including hydrologic models that use geothermal data …

The presence of weak phyllosilicates may explain the low shear strengths of fault zones if
they define well‐developed fabrics. The growth of phyllosilicates is favored in meteoric water …

At depths greater than several kilometers in the crust, elevated temperature, elevated
confining pressure, and the presence of reactive pore fluids typically drive rapid destruction …

The internal structures of the Wattle Gully Fault provide insights about the mechanics and
dynamics of fault systems exhibiting fault valve behavior in high fluid pressure regimes. This …

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 …

Abstract Comparison of mass transfer patterns, geometry and microstructures developed
within and around veins allows the interpretation of processes of fluid flow during …

An assessment of F-C1-OH partitioning between natural apatite and biotite in a variety of
rocks was used to evaluate reciprocal (Mg, Fe 2+, Al VI)(F, Cl, OH) mixing properties for …

Liberation of iron and potassium by widespread postmetamorphic albitization of country
rocks was one of the likely contributing processes in the formation of both barren and …