WebIn this issue, two studies are presented on the African craton, which give complementary insights into the formation of Gondwana and the importance of subduction processes during this event. Triantafyllou et al. (this issue) report new mapping, tectonic, metamorphic and U–Pb zircon data on polyphased arc-related units within the Moroccan Pan ... WebThe East African Orogeny at ~650–630 Mya affected a large part of Arabia, north-eastern Africa, East Africa and Madagascar. Collins and Windley (2002) propose that in this …
Mozambique Belt - Wikipedia
WebThe Mozambique Belt is a band in the earth's crust that extends from East Antarctica through East Africa up to the Arabian-Nubian Shield. It formed as a suture between plates during the Pan-African orogeny, when Gondwana was formed. WebApr 10, 2024 · Reconstructing the origin of Minoa with detrital zircons: Did Minoa derive from Gondwana-Land or Laurentia? flameshot source
Pan-African orogeny - Wikipedia
WebNov 30, 2024 · It is located near Lake Tanganyika in Burundi, along the western branch of the East African Rift. Field observations suggest that the mineralized veins formed in the upper crust. Previous structures inherited from the Kibaran orogeny may have been reused during the mineralizing event. The paragenetic sequence and the geochronological data … WebDec 21, 2024 · Abstract The modern vegetation of East Africa is a complex mosaic of rainforest patches; small islands of tropic-alpine vegetation; extensive savannas, ranging from almost pure grassland to wooded savannas; thickets; and montane grassland and forest. Here I trace the evolution of these vegetation types through the Cenozoic. WebThe worldwide 1.35-0.9 Ga cascade of continental collisions that constructed the supercontinent Rodinia is known in Africa as the Kibaran orogeny. Effects of this can be found along the margins of the Central and Southern Africa Cratons. Kibaran events did not affect the West African Craton. flameshot screenshot