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Jingsui Yang

Researcher at Nanjing University

Publications -  211
Citations -  8240

Jingsui Yang is an academic researcher from Nanjing University. The author has contributed to research in topics: Ophiolite & Mantle (geology). The author has an hindex of 48, co-authored 195 publications receiving 6813 citations. Previous affiliations of Jingsui Yang include Ontario Ministry of Natural Resources & Carma.

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Geology - Oblique stepwise rise and growth of the Tibet plateau

TL;DR: In this article, the authors propose two end member models of how the high elevations in Tibet formed: (i) continuous thickening and widespread viscous flow of the crust and mantle of the entire plateau and (ii) time-dependent, localized shear between coherent lithospheric blocks.
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Diamond- and coesite-bearing chromitites from the Luobusa ophiolite, Tibet

TL;DR: In this paper, the authors reported the occurrence of diamond as an inclusion in OsIr alloy and coesite as part of a silicate assemblage rimming a grain of FeTi alloy, both of which were recovered from chromitite.
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Compositions of chromite, associated minerals, and parental magmas of podiform chromite deposits: The role of slab contamination of asthenospheric melts in suprasubduction zone environments

TL;DR: In this paper, the authors proposed a new model in which chromitite formation was involved in intra-oceanic subduction zones initiated in closing oceanic basins, where the upward flow changes from vertical to subhorizontal and velocity is greatly reduced.
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Discovery of an eclogite belt in the Lhasa block, Tibet: A new border for Paleo-Tethys?

TL;DR: A newly discovered eclogite belt in the eastern part of the Lhasa Block, Tibet, is about 500-1000m wide and at least 60 km long in an E-W direction as discussed by the authors.
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Metamorphic evolution of the coesite-bearing ultrahigh-pressure terrane in the North Qaidam, Northern Tibet, NW China

TL;DR: Wang et al. as discussed by the authors showed that the Dulan region is a UHP metamorphic terrane, and the peak conditions of the NDB eclogites are P = 2.9-3.2 GPa, and T = 631-687°C.