Tectonic evolution of the eastern margin of the Tibetan plateau: Insight from crustal structures using P wave receiver functions
Journal of Asian Earth Sciences(2020)
Abstract
•We study crustal thickness and velocities in the eastern margin of the Tibetan plateau.•There is a significant Moho step beneath the Longmenshan fault zone.•Low velocity anomalies are notable in the mid-lower crust beneath the plateau.•Ancient deformation is clear in the crust beneath the Sichuan Basin.
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Key words
Tibetan Plateau,Sichuan Basin,Lower crustal flow
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