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The notion that Gondwana was assembled during the Late Precambrian from two older fragments along the Pan-African Mozambique Belt was first proposed in the early 1980s. [3] A decade later this continental collision was named the East African Orogeny, but it was also realised that this was not the simple bringing together of two halves.
Gondwana (/ ɡ ɒ n d ˈ w ɑː n ə /) [1] was a large landmass, sometimes referred to as a supercontinent.The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia, Zealandia, Arabia, and the Indian Subcontinent.
Famatinian arc magmatism was caused by the subduction of Iapetus Ocean lithosphere beneath Gondwana. [8] As subduction went on, the peak of the orogeny resulted from the collision of the Cuyania terrane with Pampia in the Ordovician. [12] It has been suggested that the coeval Appalachian Taconic orogeny is the "northward" continuation of the ...
The Damara Belt is exposed in Namibia between the Congo and Kalahari cratons and continues southwards into the coastal Gariep and Saldania Belts and northwards into the Kaoko Belt. It is the result of closure of the Adamastor and Damara oceans and includes two horizons associated with a severe equator-ward glaciation explained by the Snowball ...
The Gondwanide orogeny was an orogeny active in the Permian that affected parts of Gondwana that are by current geography now located in southern South America, South Africa, Antarctica, Australia and New Guinea. [1] The zone of deformation in Argentina extends as a belt south and west of the cratonic nucleus of Río de la Plata–Pampia. [2]
The Cimmerian orogenic belt in Greece comprises the Serbomacedonian, Circum Rhodope, Axios, Pelagonian and Rhodope zones, while the Bayburt, Sinop, Kirklareli and Sakarya zones are situated in Turkey. The Alpine orogenic belt includes Neo-Tethys oceanic sedimentary rocks, the Pindos-Subpelagonian ophiolites and the External Hellenides.
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