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Southern Africa showing location of Zimbabwe Craton

The Zimbabwe Craton is an area in Southern Africa of ancient continental crust, being a part of the ancient continent of Western Gondwana, with rocks dating back to the early Archean Eon, possibly as early as 3.46 billion years ago (Ga.).[1] The craton is named after the country of Zimbabwe where the majority of the craton is. The rocks of the Zimbabwe Craton are separated from the rocks of the Kaapvaal Craton to the southeast by the 250 kilometres (160 mi) wide Limpopo Belt of granulite facies tectonites. The Limpopo belt formed contemporaneously with the Zimbabwe and Kaapvaal cratons, but remained geologically active until much later. It was only in the late Archean, ca. 2.8-2.5 Ga., that the two cratons were stabilized together and that high-grade metamorphism ceased in the Limpopo Belt. North of the Zimbabwe Craton is the Zambezi Belt.[2]

Origin[edit]

The Zimbabwe Craton formed from the suture of two smaller blocks, the Tokwe Segment to the south and the much smaller Rhodesdale Segment (aka Rhodesdale gneiss), to the north. The rocks of these segments have been dated to as early as 3.46 Ga.[1] The Tokwe Segment probably stabilized about 3.3 Ga., and there is evidence that the Rhodesdale Segment stabilized about the same time.[3][4]

The synchroneity and extent of the Tokwe Segment is considered strong evidence supporting a predominantly intra-cratonic origin for the Late Archaean greenstone belts of Zimbabwe and refuting an arc accretion origin for the craton.[4]

References[edit]

  1. ^ a b Wilson, J. F.; Nesbitt, R. W. & Fanning, C. M. (1995). "Zircon geochronology of Archaean felsic sequences in the Zimbabwe Craton: a revision of greenstone stratigraphy and a model for crustal growth". In Coward, M. P. & Ries, A. C. (eds.). Early Precambrian processes. Geological Society Special Publications, issue 95. London: Geological Society of London. pp. 109–126. ISBN 978-1-897799-36-9.
  2. ^ Jelsma, H. A. and Dirks, P. H. G. M. (2002). "Neoarchean Tectonic Evolution of the Zimbabwe Craton". In Fowler, C. M. R.; Ebinger, C. L.; Hawkesworth, C. J. (eds.). The Early Earth: Physical, Chemical and Biological Development. Geological Society Special Publications, issue 199. London: Geological Society of London. pp. 183–211. ISBN 978-1-86239-109-3.{{cite book}}: CS1 maint: multiple names: authors list (link)
  3. ^ Dirks, P. H. G. M. and Jesma, H. A. (2002). "Crust–mantle decoupling and the growth of the Archaean Zimbabwe Craton". Journal of African Earth Sciences. 34 (3–4): 157–166. Bibcode:2002JAfES..34..157D. doi:10.1016/s0899-5362(02)00015-5.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  4. ^ a b Blenkinsop, T. G.; Martin, A.; Jelsma, H. A. & Vinyu, M. L. (1997). "The Zimbabwe Craton". In de Wit, M. J. & Ashwal, L. D. (eds.). Greenstone Belts. Oxford, England: Clarendon Press. pp. 567–580. ISBN 978-0-19-854056-4.
source: https://en.wikipedia.org/wiki/Zimbabwe_Craton

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