For geothermal pourposes I am researching waters related to Cretaceous limestone-dolostomes and sandstones not too far of an inverse fault. The temperature at surface conditions is of 19 ºC (water for drill after 24 hours of pumping) that is quasi equal at the temperature estimated using the local geotherm, but I get a reservoir temperatura of 39 ºC using the silica-quart geothermomer. The Saturation index of quartz is oversaturated =0.35.