2000
DOI: 10.1130/0091-7613(2000)028<0939:rkdtis>2.3.co;2
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Rift kinematics during the incipient stages of continental extension: Evidence from the nascent Okavango rift basin, northwest Botswana

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Cited by 62 publications
(121 citation statements)
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“…2 used below for analysis of large-scale salt balance). A variety of hydrological, geochemical, sedimentological and biological processes have shaped the Delta over a range of spatial and temporal scales (Hutchins et al, 1976;Ellery et al, 1993b;McCarthy and Ellery, 1994;Modisi et al, 2000;Gumbricht et al, 2001). One key feature of the Okavango Delta is its strong seasonality, which is due to the highly variable flow in the Okavango River.…”
Section: The Okavango Deltamentioning
confidence: 98%
“…2 used below for analysis of large-scale salt balance). A variety of hydrological, geochemical, sedimentological and biological processes have shaped the Delta over a range of spatial and temporal scales (Hutchins et al, 1976;Ellery et al, 1993b;McCarthy and Ellery, 1994;Modisi et al, 2000;Gumbricht et al, 2001). One key feature of the Okavango Delta is its strong seasonality, which is due to the highly variable flow in the Okavango River.…”
Section: The Okavango Deltamentioning
confidence: 98%
“…Thus, details of the structural and tectonic development of the ORZ are limited (e.g., Scholz et al, 1976;McCarthy et al, 1993;Modisi, 2000;Modisi et al, 2000;Gumbricht et al, 2001). This study has circumvented this problem by employing high resolution aeromagnetic and gravity surveys that provides an unprecedented view of the basement geology and permits us to: (1) evaluate the role of pre-existing basement fabric on the rift development, (2) map the distribution of faults and determine their displacements, and (3) provide insights into the 2D shallow subsurface geometry and basin development of the ORZ.…”
Section: Introductionmentioning
confidence: 99%
“…This work describes diagenesis in mapped Okavango alluvial fan and adjacent dune siliclastic sediments in the western MOZ (MakgadikgadiOkavango-Zambezi) basin in northern Botswana. The sediments lie in flat though down faulted terrain within a southwestern extension of the East African rift (EAR, Modisi et al, 2000). Subsidence was reactivated approximately 2.4-5.0 Ma along NE-SW trends (Kampunzu et al, 1998;Tiercelin and Lezzar, 2002).…”
Section: Introductionmentioning
confidence: 99%