The Cimmerian Orogeny was an orogeny that created mountain ranges that now lie in Central Asia. The orogeny is believed to have begun during the Late Triassic about 240–200 million years ago, when parts of the Cimmerian continent collided with the southern coast of Kazakhstania and North and South China, closing the ancient Paleo-Tethys Ocean between them.[1] Blocks that derive from that continent now form part of Turkey, Iran, Tibet and western Southeast Asia. Much of the plate's northern boundary formed mountain ranges that were as high as the present-day Himalayas.
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Plate Tectonics 600Ma to Today by CR Scotese
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Celal Şengör Daşgil Palçıq Vulkanlarında | ADNSU da görüş | Mineralogiya muzeyi | SEG ASOIU
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See also
- Hercynian orogeny - an orogeny that preceded the Cimmerian orogeny
- Alpine orogeny - an orogeny that succeeded the Cimmerian orogeny
References
- ^ Golonka, J.; Embry, A.; Krobicki, M. (2018). "Late Triassic Global Plate Tectonics" (PDF). In Tanner, L. (ed.). The Late Triassic World. Topics in Geobiology. Vol. 46. Springer International. doi:10.1007/978-3-319-68009-5_2. ISBN 978-3-319-68008-8.
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This page was last edited on 22 July 2023, at 21:54