Fig. 5From: Evaluation of the Lund deep geothermal exploration project in the Romeleåsen Fault Zone, South Sweden: a case studyIllustration of the DGE-1 well design [Modified from Howard-Orchard (2003)]. Perforations in the sedimentary succession between 1427 and 1905 m were conducted after the testing and evaluation of the crystalline basement. The results from the testing of the sedimentary succession are presented in Rosberg (2006, 2007)Back to article page