The permeability of many rocks and ores is low but can increase dramatically during fluid-rock interaction via formation of connected porosity induced by mineral replacement...
Measured cation, anion, and silica are presented as well as calculations evaluating mass balance performed for 4 fracture sustainability tests under EGS conditions: Stripa granite, Metamudstone, Rhyol
Data set corresponding to the figures shown in the submitted paper "Recent advances in characterizing water weakening and fluid-rock interaction processes in porous rocks"by Davide Geremia, Christian
Understanding seismotectonic activity preceding major earthquakes is key to clarifying fault mechanics and improving hazard assessment. We investigate interseismic geodetic data and premainshock seism
