Modelo de favorabilidad geotérmica mediante Play Fairway Analysis de la zona geotérmica dentro del Complejo Caldera de Acoculco (Puebla, México)
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Resumen
En este trabajo se presentan los resultados de un Play Fairway Analysis realizado en la zona geotérmica localizada dentro del Complejo Caldera de Acoculco. En este estudio, considerando la existencia probada de una anomalía geotérmica en el subsuelo (identificada con pozos de >1.5 km de profundidad), se han utilizado datos geocientíficos de estudios previos considerados como indicadores o proxies de permeabilidad para generar el modelo de favorabilidad geotérmica. Este Play Fairway Analysis tiene un enfoque de expertos (expert-driven), debido a que no existen pozos con recursos geotérmicos probados para realizar un Play Fairway Analysis basado en datos (data-driven). Los datos empleados en este análisis fueron la ubicación de las fallas, del flujo de CO2, de los manantiales, de la temperatura del suelo, de los depósitos de ópalo y de los cráteres de erupciones hidrotermales. Las capas de los datos (evidence layers) fueron manejadas e integradas usando el software QGIS®. Los resultados muestran dos zonas con mayor favorabilidad geotérmica, ubicadas a aproximadamente 200 m al noroeste del pozo exploratorio EAC-1 y en la zona conocida como Alcaparrosa. En este trabajo, gracias a la recopilación de datos, también se discute por qué la zona geotérmica de Acoculco podría ser un sistema geotérmico convectivo y cómo las zonas con mayor favorabilidad geotérmica resultantes son las que tienen mayor potencial para alojar fluidos geotérmicos.
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