Figure 5From: Three-dimensional thermal sensitivity analysis of cooling of a magma chamber in the Los Azufres geothermal field, Michoacán, MexicoSimulated temperatures and temperature excess values. Actual simulated temperature (open diamonds) and temperature excess (difference between the simulated temperature and normal geothermal gradient temperature; filled diamonds) are reported for the model M55 (magma chamber at 5 km depth, 600 km3 volume, and emplacement time of the 100,000 years with δt of 500 years).Back to article page