A two-dimensional temperature field simulation of the La Primavera geothermal area, México

•Conductive 2D thermal profiles show the subsurface temperature distribution.•A developed numerical simulator code calculates the thermal profiles.•Temperatures of 320-540 °C occur at depths of 3000 m within the granitic basement.•The natural thermal state model of La Primavera provides new scenario...

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Veröffentlicht in:	Geothermics 2021-11, Vol.96, p.102201, Article 102201
Hauptverfasser:	Espinoza-Ojeda, O.M., Macías, J.L., Gómez-Arias, E., Muñiz-Jauregui, J.A., Rivera-Calderón, E., Figueroa-Soto, A.G., Vázquez-Rosas, R., Garduño-Monroy, V.H.
Format:	Artikel
Sprache:	eng
Schlagworte:	Algorithms Boundary conditions Calderas Exploitation Exploration Formation temperatures Geology Geophysics Geothermal power Geothermal resources Heat Heat flow Heat transfer Heat transmission High temperature La Primavera Lithology Mathematical models México Numerical models Power plants Stratigraphy Temperature Temperature distribution Temperature profiles Thermal conductivity Thermal profiles Two dimensional models Well drilling
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