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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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Highly fractionated Jurassic I-type granites and related tungsten mineralization in the Shirenzhang deposit, northern Guangdong, South China: Evidence from cassiterite and zircon U-Pb ages, geochemistry and Sr-Nd-Pb-Hf isotopes

TL;DR: In this paper, the authors reported new cassiterite U-Pb ages and Pb isotopes of sulfides for the Shirenzhang tungsten deposit, combined with new zircon UPb dates and Hf isotopes, elemental geochemistry and Sr-Nd-pb isotope of the concealed granitic rocks, with aims to elucidate the origin of the ore-related granites and the link between the tengsten mineralization and granitic magmatism.
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Geochronology, elemental and Nd–Hf isotopic geochemistry of Devonian A-type granites in central Jiangxi, South China: Constraints on petrogenesis and post-collisional extension of the Wuyi–Yunkai orogeny

TL;DR: In this paper, the authors reported a systematic study on two Devonian A-type granites in the central Jiangxi Province, which indicated that the Wuyi-Yunkai orogeny in South China had changed from syncollisional crustal thickening to post-collisionally extension at least from 415-Ma.
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Late Mesozoic magmatism of the Jiurui mineralization district in the Middle-Lower Yangtze River Metallogenic Belt, Eastern China: Precise U-Pb ages and geodynamic implications

TL;DR: Zhang et al. as discussed by the authors carried out precise and detailed zircon U-Pb dating for all types of magmatic rocks from the Wushan ore deposit in the Jiurui district.
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Reliability of LA-ICP-MS U-Pb dating of zircons with high U concentrations: A case study from the U-bearing Douzhashan Granite in South China

TL;DR: In this article, the authors carried out a SHRIMP U-Pb dating for high-U zircons and the results showed that the high U (12,007-26,706) rim domains of the zirons always yield older 206 Pb/ 238 U ages than the low-U (558-3667) mantle domains (228,±-11,Ma, n = 4, MSWD = 3.1), and both of these ages are older than the emplacement age (211 ǫ± ǔ 3 �