Fig. 7From: Modelling of flow through naturally fractured geothermal reservoirs, Taupō Volcanic Zone, New ZealandComparison of pressure distributions in continuum and DFN models for, from top to bottom rows: models A, B, D and C2. From left to right: example of backbone network; input P10; DFN with 1 realisation; average of 50 DFN realisations; Equivalent Continuum Models (ECM). The white dashed lines on the plots for Models B, D and C2 indicate changes in lithology in the modelsBack to article page