H
Hai Jiang
Researcher at China University of Geosciences (Wuhan)
Publications - 13
Citations - 238
Hai Jiang is an academic researcher from China University of Geosciences (Wuhan). The author has contributed to research in topics: Zircon & Petrogenesis. The author has an hindex of 5, co-authored 10 publications receiving 142 citations.
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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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Geochronological, geochemical and Sr-Nd-Hf isotopic constraints on the petrogenesis of Late Cretaceous A-type granites from the Sibumasu Block, Southern Myanmar, SE Asia
TL;DR: In this paper, a detailed study on geochronology, elemental and Sr-Nd-Hf isotopic geochemistry for the Hermyingyi and Taungphila granites in southern Myanmar is presented, with the aim of determining their petrogenesis and tectonic implications.
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Spatiotemporal distribution, geological characteristics and metallogenic mechanism of tungsten and tin deposits in China: An overview
Shao-Yong Jiang,Kui-Dong Zhao,Hai Jiang,Huimin Su,Suo-Fei Xiong,Yi-Qu Xiong,Yaoming Xu,Wei Zhang,Lüyun Zhu +8 more
TL;DR: The formation of tungsten and tin in China spans a large period of time, from Proterozoic to Cenozoic, but the Mesozoic Yanshanian mineralization is the most important as mentioned in this paper.
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Fluid inclusion and isotopic (C, H, O, S and Pb) constraints on the origin of late Mesozoic vein-type W mineralization in northern Guangdong, South China
TL;DR: In this paper, a detailed study on fluid inclusions and C-H-O-S-Pb isotopic analyses of mineral separates for these three deposits, in order to resolve the origin and evolution of ore-forming fluids and the ore deposition mechanism was carried out.
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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.