Cenozoic reactivation along the Late Triassic Ganzi-Litang suture, eastern Tibetan Plateau
Abstract
The spatial-temporal development of Cenozoic reactivation along Mesozoic suture zones in the Tibetan Plateau are first-order parameters needed for assessing models of plateau growth. The Ganzi-Litang suture, in the eastern Tibetan Plateau, developed in the Late Triassic because of subduction and closure along the eastern branch of the Paleo-Tethys Ocean. Near the city of Litang, the Ganzi-Litang suture is defined by a mélange sequence with...
Paper Details
Title
Cenozoic reactivation along the Late Triassic Ganzi-Litang suture, eastern Tibetan Plateau
Published Date
May 1, 2020
Journal
Volume
11
Issue
3
Pages
1069 - 1080
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