Fig. 3From: Synthetic modelling of downhole resistivity data to improve interpretation of basin morphology from magnetotelluric inversionSimplified stratigraphy for relevant units of the Georgina and Eromanga Basins. Modified after Greene (2010) with data from Ambrose et al. (2001), Draper (2007) and Kruse et al. (2013). Grey units are predominantly limestone, and white units are siliciclastic. Starred units intersected by boreholes Todd 1, Bradley 1 or Beantree 1 shown in Fig. 1Back to article page