Paleo-Tethys system and accretionary orogen in the Tibet Plateau
Abstract
The Paleo-Tethys system in the Tibet Plateau formed under environment of multi-ocean basins,micro-terrains ( ribben continents) ,island arcs,subductions and collisions. Its architectures include four ophiolite or ophiolitic melange belts representing Paleo-Tethysoceanic crustal relics ( South Kunlun-Animaqen ophiolite zone,Jinshajiang-Ailaoshan-Songma ophiolite zone,Central Qiangtang-Lancangjiang-Changning Menglian ophiolite zone and Songduo...
Paper Details
Title
Paleo-Tethys system and accretionary orogen in the Tibet Plateau
Published Date
Jan 1, 2013
Journal
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