Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction
Abstract
null null Integration of lithostratigraphic, magmatic, and metamorphic data from the Lhasa–Qiangtang collision zone in central Tibet (including the Bangong suture zone and adjacent regions of the Lhasa and Qiangtang terranes) indicates assembly through divergent double sided subduction. This collision zone is characterized by the absence of Early Cretaceous high-grade metamorphic rocks and the presence of extensive magmatism with enhanced mantle...
Paper Details
Title
Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction
Published Date
Feb 15, 2016
Journal
Volume
245
Pages
7 - 17
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