J
Juhn G. Liou
Researcher at Stanford University
Publications - 301
Citations - 22240
Juhn G. Liou is an academic researcher from Stanford University. The author has contributed to research in topics: Metamorphism & Eclogite. The author has an hindex of 83, co-authored 301 publications receiving 21042 citations. Previous affiliations of Juhn G. Liou include Tokyo Institute of Technology & China University of Geosciences (Wuhan).
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Blueschists and Eclogites of the World and Their Exhumation
TL;DR: In this paper, the authors classified high-P/T metamorphic belts into two types: collision-type and cordilleran-type blueschists, based on their protoliths.
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Coesite-bearing eclogite from the Dabie Mountains in central China
TL;DR: Coesite and Coesite pseudomorphs are recognized in eclogite from the Dabie Mountains, a collision zone between the Sino-Korean and Yangtze cratons in central China as discussed by the authors.
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An outline of the plate tectonics of China
TL;DR: In this paper, the Junggar-Hegen suture is used to detect ophiolites and rare blueschists in the Cathaysian suture, and the presence of bluechists reveals evidence of large-scale subduction and tectonic exhumation during consolidation of the Eurasian plate.
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Global UHP metamorphism and continental subduction/collision: The himalayan model
TL;DR: More than 20 recognized ultrahigh pressure (UHP) terranes have been documented; these occurrences demonstrate that not only is continental crust subducted to depths as great as 150 km, but also that some supracrustal rocks were then exhumed to the earth's surface as mentioned in this paper.
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Zircon as the best mineral for P-T-time history of UHP metamorphism: A review on mineral inclusions and U-Pb SHRIMP ages of zircons from the Dabie-Sulu UHP rocks
F.L. Liu,Juhn G. Liou +1 more
TL;DR: Zircon is the best mineral to record the complex evolution history of ultrahigh pressure (UHP) metamorphic rocks as mineralogical and geochemical tracers of UHP metamorphism are almost obliterated in matrix assemblages resulted from subsequent retrogression during exhumation as discussed by the authors.