Evaluation of geothermal flow at the springs in Aragon (Spain), and its relation to geologic structure

摘要

The geothermal flow which emerges by convection at the springs in Aragon is evaluated, and compared with the theoretical heat flow which permeates the surface of the region by conduction. The geological materials through which the convection takes place are defined (geothermal formations), and the areas where thermal convection appears most intensely are related.