Loss of well productivity due to the formation of minerals blocking permeable channels is a common problem in geothermal fields. (Read more)
Environmental changes in the subsurface can be tracked by the fluid-rock interactions and the resulting hydrothermal alteration. (Read more)
Fluid is contained in and travels in voids in rock, such as pore spaces, mineral defects, micro-fractures or fractures. (Read more)
Identifying sites of boiling within a geothermal reservoir provides valuable information as to the location of high temperature fluids. (Read more