Normal faulting in central Tibet since at least 13.5 Myr ago

Tectonic models for the evolution of the Tibetan plateau interpret observed east–west thinning of the upper crust to be the result of either increased potential energy of elevated crust 1 or geodynamic processes that may be unrelated to plateau formation 2 , 3 , 4 , 5 , 6 . A key piece of informatio...

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