L
Li Su
Researcher at China University of Geosciences (Beijing)
Publications - 81
Citations - 5419
Li Su is an academic researcher from China University of Geosciences (Beijing). The author has contributed to research in topics: Zircon & Subduction. The author has an hindex of 37, co-authored 66 publications receiving 4192 citations. Previous affiliations of Li Su include Northwestern University & China University of Geosciences (Wuhan).
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Tectonics of the North Qilian orogen, NW China
TL;DR: The Qilian Orogen at the northern margin of the Tibetan Plateau is a type suture zone that recorded a complete history from continental breakup to ocean basin evolution, and to the ultimate continental collision in the time period from the Neoproterozoic to the Paleozoic.
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Evolution from Oceanic Subduction to Continental Collision: a Case Study from the Northern Tibetan Plateau Based on Geochemical and Geochronological Data
TL;DR: Two apparently distinct, sub-parallel, paleo-subduction zones can be recognized along the northern margin of the Tibetan Plateau: the North Qilian Suture Zone (oceanic-type) with ophiolitic melanges and high-pressure eclogites and blueschists in the north, and North Qaidam Belt (continental type) in the south, an ultrahighpressure (UHP) metamorphic terrane comprising pelitic and granitic gneisses, eclogs and garnet peridotites as discussed by the authors.
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Continental orogenesis from ocean subduction, continent collision/subduction, to orogen collapse, and orogen recycling: The example of the North Qaidam UHPM belt, NW China
TL;DR: The North Qaidam ultra-high pressure metamorphic (UHPM) belt in the northern Tibetan Plateau records a complete history of the evolution of a continental orogen from prior seafloor subduction, to continental collision and subduction.
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Geochronology of diamond-bearing zircons from garnet peridotite in the North Qaidam UHPM belt, Northern Tibetan Plateau: A record of complex histories from oceanic lithosphere subduction to continental collision
TL;DR: In this paper, the results of a comprehensive study of zircons separated from the Luliangshan peridotite massif within the 400km-long North Qaidam UHPM belt, northern Tibetan Plateau, NW China were reported.
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Tracing the 850-Ma continental flood basalts from a piece of subducted continental crust in the North Qaidam UHPM belt, NW China
TL;DR: In this article, the Yuka eclogite terrane has been used to infer the origin of the Rodinia supercontinent at ∼850 million years ago (Ma).