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Shao-Yong Jiang

Researcher at China University of Geosciences (Wuhan)

Publications -  120
Citations -  1772

Shao-Yong Jiang is an academic researcher from China University of Geosciences (Wuhan). The author has contributed to research in topics: Zircon & Fluid inclusions. The author has an hindex of 16, co-authored 119 publications receiving 941 citations. Previous affiliations of Shao-Yong Jiang include Nanjing University.

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Early Jurassic mafic dykes from the Aigao uranium ore deposit in South China: Geochronology, petrogenesis and relationship with uranium mineralization

TL;DR: In this paper, apatite U-Pb dating, whole-rock major and trace element and Sr-Nd-pb isotope analysis were conducted for the dolerite dykes from the Aigao uranium ore deposit.
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Hydrothermal evolution and ore genesis of the Zhaiping Ag-Pb-Zn deposit in Fujian Province of Southeast China: Evidence from stable isotopes (H, O, C, S) and fluid inclusions

TL;DR: The Zhaiping Ag-Pb-Zn mine is a typical mesothermal deposit that formed in an extensional environment related to the early Cretaceous subduction of the paleo-Pacific plate as discussed by the authors.
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Timing and Source of the Hermyingyi W-Sn Deposit in Southern Myanmar, SE Asia: Evidence from Molybdenite Re-Os Age and Sulfur Isotopic Composition

TL;DR: In this paper, the Hermyingyi W-Sn deposit in southern Myanmar, SE Asia, is identified as a typical quartz-vein type W-sn deposit with Re-Os model ages ranging from 67.8±1.6 to 69.2± 1.2 Ma and a well defined isochron age of 68.4±2.5 Ma.
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Chemical and boron isotopic compositions of tourmaline at the Dachang Sn-polymetallic ore district in South China: Constraints on the origin and evolution of hydrothermal fluids

TL;DR: In this article, the major, trace element, and boron isotopic compositions of different types of tourmaline in the Dachang ore district were investigated. But the results of the study were limited.
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Cretaceous granitic magmatism and mineralization in the Shanhu W-Sn ore deposit in the Nanling Range in South China

TL;DR: Zhang et al. as mentioned in this paper showed that the Yantianling S-type granite and associated W-Sn mineralization in the Nanling Range were formed during the regional lithospheric extensional environment.