Tibetan, Variscan, and Precambrian Basement Reactivation: Products of Continental Collision

@article{Dewey1973TibetanVA,
  title={Tibetan, Variscan, and Precambrian Basement Reactivation: Products of Continental Collision},
  author={John Frederick Dewey and Kevin C. Burke},
  journal={The Journal of Geology},
  year={1973},
  volume={81},
  pages={683 - 692}
}
Extensive terranes of basement reactivation are interpreted as resulting from crustal thickening following continental collision. It is suggested that terranes, such as the Grenville Province and much of the Variscan orogenic belt in Europe, have their modern analog in the Tibetan Plateau. The Tibetan Plateau is underlain by a continental crust between 60 and 80 km thick and is characterized by extensive high-potash Neogene vulcanism. Following T. H. Green's arguments that partial melting of a… Expand
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