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Table 5 Matrix permeability values are shown below which the flow regime noted to its right is possible

From: Hydraulic behavior of fault zones in pump tests of geothermal wells: a parametric analysis using numerical simulations for the Upper Jurassic aquifer of the North Alpine Foreland Basin

  1. The table has been derived from the corresponding regression functions for minimum and maximum values of specific fault and matrix storage and for a fault permeability of 1.0e−9 m2