Circulation des fluides en zones de failles

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Il est généralement admis que les fractures constituent des voies importantes pour l’écoulement des fluides dans la croûte terrestre.

Les Zones de Failles Crustales sont des zones naturellement perméables et profondes permettant aux fluides de localiser des anomalies positives de température à des profondeurs potentiellement exploitables.

La modélisation numérique de processus physiques permet de comprendre les facteurs susceptibles d’influencer la circulation des fluides et d’estimer la profondeur et l’intensité des anomalies de température.
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