volume 47, issue 2, P2.28-2.37 2006
DOI: 10.1111/j.1468-4004.2006.47228.x
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Abstract: In her RAS PresidentialAddress for 2005, Kathryn A Whaler discusses how mapping the electrical resistivity of the subsurface can be used to investigate continental rifting, with examples from Africa. 1: Karoo sedimentary basins within the mobile belts of southern Africa. Basins 1-4 lie within the Damara orogenic belt, which extends west of the map area into Namibia, and 3 and 4 are the basins studied here. The contours indicate approximate basement. Basins are: 1 Passarge, 2 Mid-Zambezi, 3 Mana Pools, 4 Lower…

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