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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.
English: Approximate positions of Siberia, Gondwana, North and South China, Baltica and smaller terranes in the middle Cambrian (c. 500 Ma). AN: Annamia, CM: Central ...
Gondwana Research is a peer-reviewed scientific journal with an "all earth science" scope and an emphasis on the origin and evolution of continents. It is part of the Elsevier group, published by Journal Center, China University of Geosciences Beijing, 29 Xueyuan Road, Beijing 100083, China.
Location of the Paleo-Tethys Ocean circa ~250 million years ago Location of the Paleo-Tethys Ocean circa 380 million years ago [1]. The Paleo-Tethys or Palaeo-Tethys Ocean was an ocean located along the northern margin of the paleocontinent Gondwana that started to open during the Middle Cambrian, grew throughout the Paleozoic, and finally closed during the Late Triassic; existing for about ...
The Tien Shan terrane maintained a biogeographic affinity with Gondwana, [61] and the Alborz margin of Gondwana was linked biogeographically to South China. [62] Southeast Asia's fauna also maintained strong affinities to Gondwana's. [63] North China was biogeographically connected to Laurentia and the Argentinian margin of Gondwana. [64]
The North China University of Technology (北方工业大学) is a municipal public university in Shijingshan, Beijing, China. It is affiliated with the City of Beijing and funded by the municipal government. The predecessor was the national Beiping advanced industrial vocational school, founded in 1946.
Gondwana University is a university established in 2011 in the city of Gadchiroli in Maharashtra state in central India. [1] It is named after Gondwana region in ...
The North China Craton collided with Siberia by the Jurassic, completely closing the Proto-Tethys Ocean. [38] By the Early Permian, the Cimmerian plate split from Gondwana and moved towards Laurasia, thus closing the Paleo-Tethys Ocean and forming the Tethys Ocean in its southern end. Most of the landmasses were all in one.