Central African Shear Zone

From Wikipedia, the free encyclopedia
Jump to: navigation, search
Central Africa showing CASZ
Rifts in Sudan and Kenya

The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE direction from the Gulf of Guinea through Cameroon into Sudan.[1] The structure is not well understood. As of 2008 there was still no general agreement about how the individual shears along the lineament link up.[2]

Description[edit]

The shear zone dates to at least 640 MA (million years ago).[3] Motion occurred along the zone during the break-up of Gondwanaland in the Jurassic and Cretaceous ages.[1] Some of the faults in the zone were rejuvenated more than once before and during the opening of the South Atlantic in the Cretaceous era.[3]

The Pernambuco fault in Brazil is a continuation of the shear zone to the west.[3] In Cameroon, the CASZ cuts across the Adamawa uplift, a post-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south.[4] Volcanic activity has occurred along most of the length of the Cameroon line from 130 MA to the present, and may be related to re-activation of the CASZ.[5] The lithosphere beneath the CASZ in this area is thinned in a relatively narrow belt, with the asthenosphere upwelling from a depth of about 190 km to about 120 km.[6] The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad.[3]

Sudan[edit]

The CASZ was formerly thought to extend eastward only to the Darfur region of western Sudan.[3] It is now known to extend into central and eastern Sudan, with a total length of 4,000 km.[1] In the Sudan, the shear zone may have acted as a structural barrier to development of deep Cretaceous-Terriary sedimentary basins in the north of the area. Objections to this theory are that the Bahr el Arab and Blue Nile rifts extend northwest beyond one proposed line for the shear zone.[7] However, the alignment of the northwestern ends of the rifts in this areas supports the theory.[8]

References[edit]

  1. ^ a b c Ibrahim, Ebinger & Fairhead 1996, pp. 79–97.
  2. ^ Pankhurst 2008, pp. 404.
  3. ^ a b c d e Dorbath et al. 1986, pp. 751-766.
  4. ^ Schlüter & Trauth 2008, pp. 60.
  5. ^ Foulger & Jurdy 2007, pp. 16.
  6. ^ Plomerova et al. 1993, pp. 381–390.
  7. ^ Selley 1997, pp. 113.
  8. ^ Bowen & Jux 1987, pp. 143.

Sources books[edit]