The HYDROTHERM code as a tool for integrating geophysics in geothermal prospecting

The use of numerical codes in simulating geothermal reservoirs is one of the most powerful tools for integrating geology, geochemistry, and geophysics in high enthalpy geothermal research processes. This paper summarizes some examples of USGS HYDROTHERM code application results on the islands of Gran Canaria, Lanzarote, and Tenerife, which are considered very different geothermal models. The first island has normal geothermal gradient, the second has magmatic bodies near the surface and Tenerife has a comparison between geophysical techniques to determine the recharge-discharge flows of the Cañadas-Teide system. In the first two islands there are boreholes that allow adjusting and validating the models, whereas Tenerife or La Palma have been studied using the same methodology but lack verification boreholes. Nevertheless, their model results are consistent with other geophysical techniques. This highlights the great potential of this code as an integrating tool for the different prospecting techniques to understand geothermal system operations and determine the most suitable location for deep exploration drilling. The significant benefit of this code is the capability to reproduce different evolutionary and casuistry models reliably using the same geological and thermal parameters for all islands.