The internal structure and geotectonic setting of the Xade and Tsetseng complexes in the western most part of the Kaapvaal Craton.

Abstract

The (Meixner and Peart, 1984)

Hydrogeological conceptual model of large and complex sedimentary aquifer systems – Central Kalahari Basin

“…The Makgadikgadi and Kalahari Lines are major thrust faults, which originated ∼2 Ga ago (Carney et al, 1994). The Kalahari Line defines the western edge of the Kapvaal Craton while the Makgadikgadi Line, the north-western edge of the Zimbabwe Craton (Carney et al, 1994;Key and Ayres, 2000;Pouliquen et al, 2008). The Tsau Line is a series of thrust faults along the strike of the Ghanzi meta-sediments (Ramokate et al, 2000).…”

Geophysical Modelling of the Molopo Farms Complex in Southern Botswana; Implications for Its Emplacement Within the 2 Ga Large Igneous Provinces of Southern and Central Africa

“…Complex to the north (Pouliquen et al, 2008). The concept of analytic signal of magnetic anomalies was developed by Nabighian (1972;.…”

Multiple data sources and integrated hydrological modelling for groundwater assessment in the Central Kalahari Basin

“…The Makgadikgadi and Kalahari Lines are major thrust faults, which originated ~2 Ga ago (Carney et al, 1994). The Kalahari Line defines the western edge of the Kapvaal Craton while the Makgadikgadi Line, the north-western edge of the Zimbabwe Craton (Carney et al, 1994;Key & Ayres, 2000;Pouliquen et al, 2008). The Tsau Line is a series of thrust faults along the strike of the Ghanzi meta-sediments (Ramokate et al, 2000).…”