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Chusi Li

Researcher at Indiana University

Publications -  169
Citations -  8667

Chusi Li is an academic researcher from Indiana University. The author has contributed to research in topics: Olivine & Sulfide. The author has an hindex of 53, co-authored 165 publications receiving 7491 citations. Previous affiliations of Chusi Li include Université du Québec & Chinese Academy of Sciences.

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Tethys tectonic evolution and its bearing on the distribution of important mineral deposits in the Sanjiang region, SW China

TL;DR: In this article, the authors provide a synthesis of tectonic evolution, magmatism and metallogeny in the Sanjiang region based on data from literatures, and provide evidence for two different events of subduction of the Proto-Tethys ocean at different locations.
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Partitioning of nickel, copper, iridium, rhenium, platinum, and palladium between monosulfide solid solution and sulfide liquid: Effects of composition and temperature

TL;DR: Partitioning of Ni, Cu, and Pt-group elements (Ir, Rh, Pt, Pd) between monosulfide solid solution and sulfide liquid has been investigated in the Fe-Ni-Cu-S system at 1000 and 1100°C and one atmosphere pressure as mentioned in this paper.
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Sulfide Saturation in Mafic Magmas: Is External Sulfur Required for Magmatic Ni-Cu-(PGE) Ore Genesis?

TL;DR: The importance of externally derived sulfur in the genesis of sulfide-rich, magmatic Ni-Cu-(platinum group element [PGE]) deposits remains a key, yet unresolved, issue as mentioned in this paper.
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Empirical equations to predict the sulfur content of mafic magmas at sulfide saturation and applications to magmatic sulfide deposits

TL;DR: In this article, the authors developed an analytical model to predict the sulfur content of mafic magma at the time of sulfide saturation based on several sets of published experimental data.
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Geology and petrology of the Voisey's Bay intrusion: reaction of olivine with sulfide and silicate liquids

TL;DR: The Voisey's Bay Ni-Cu-Co sulfide deposit is located in Eastern Labrador, and transects the 1.85 Ga collisional boundary between interbanded garnet-sillimanite and quartzo-feldspathic paragneisses (Tasuiyak gneisses) as mentioned in this paper.