Fig. 5
From: Numerical modeling of the geothermal hydrology of the Volcanic Island of Basse-Terre, Guadeloupe
Geometry used to represent the different scenarios, with the matrix rock, magma chambers (the optional second one is hatched), caprocks, vertical conduits, and horizontal layers. The boundary conditions are represented on the top by the blue line (constant pressure and temperature from initial values) and on the bottom by the yellow line (basal heat flux, 100 \(\text {mW/m}^2\))