Fig. 10From: Characterisation of the fracture- and karst-controlled geothermal reservoir below Munich from geophysical wireline and well informationProbability density estimates and corresponding box-whisker plots of the compressional wave velocity (\({{\text{v}}}_{{\text{p}}}\)). The plots are grouped by a–d lithology, based on the cutting report; e–h hyper-facies, based on the image analyses; and i–l the different wells. Outliers are values that fall outside the range of Q1 ± 1.5*IQRBack to article page