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Table 1 Emplacement conditions of magma chamber and geological properties for thermal models of the Los Azufres geothermal field (LAGF)

From: Three-dimensional thermal sensitivity analysis of cooling of a magma chamber in the Los Azufres geothermal field, Michoacán, Mexico

Physical property (units)

Emplacement of magma chamber

Emplacement conditions

 Depth of the top the chamber (d) (km)

5.0-9.0

 Depth of the chamber centroid (dc) (km)

7.000 to 12.875

 Volume (V) (km3)

300 to 600

 Thickness of the magma chamber (E) (km)

4.00 to 7.75

 Radius (r) (km)

5.0

 Magma emplacement temperature (Tcham) (°C)

1,350

Boundary conditions

 Surface temperature (Ts) (°C)

25

 Geothermal gradient (ΔTg) (°C/km)

30

Geological strata (strata 1–4 rock type)a

 Granite-granodiorite

 

  Width (km)

16.00

  Thermal conductivity (W/mK)

2.80

  Specific heat (J/kg K)

1,073

  Density (kg/m3)

2,680

 Metamorphic rocks

 

  Width (km)

1.00

  Thermal conductivity (W/mK)

2.73

  Specific heat (J/kg K)

1,050

  Density (kg/m3)

2,280

 Andesite

 

  Width (km)

2.75

  Thermal conductivity (W/mK)

1.72

  Specific heat (J/kg K)

1,151

  Density (kg/m3)

2,180

 Rhyolite

 

  Width (km)

0.25

  Thermal conductivity (W/mK)

3.44

  Specific heat (J/kg K)

1,074

  Density (kg/m3)

2,460

  1. aPhysical properties were taken from Contreras et al. (1988) and Verma and Andaverde (1996).