Late Triassic Continental Eclogite in the Central Tibetan Plateau Reveals 2500-km-long Paleo-Tethys Continental Subduction
Late Triassic Continental Eclogite in the Central Tibetan Plateau Reveals Paleo-Tethys Continental Subduction Academic Background The Tibetan Plateau is one of the youngest and highest plateaus on Earth, and its formation is closely related to the closure of the Tethys Ocean and the collision of the Indian-Eurasian plates. The Paleo-Tethys Ocean wa...