Evaluación del flujo geotérmico en manantiales de Aragón
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Abstract
The geothermal flow wich emerges by convection at the springs in Aragon is evaluated, and compared with the theoretical heat flow wich penetrates the surface of the region by conduction. The geological materials through wich the convection takes place are defined (geothermal formations), and the areas where thermal convection appears most intensely are related
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