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Wen-Qian Li
Researcher at Chinese Academy of Sciences
Publications - 10
Citations - 207
Wen-Qian Li is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Zircon & Petrogenesis. The author has an hindex of 5, co-authored 9 publications receiving 129 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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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.
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The geology, magnetite geochemistry, and oxygen isotopic composition of the Akesayi skarn iron deposit, Western Kunlun Orogenic Belt, Xinjiang, northwest China: Implications for ore genesis
TL;DR: The Akesayi skarn iron (Fe) deposit is hosted by the Huangyangling Group within the Tianshuihai Terrane of the Western Kunlun orogenic belt, Xinjiang, China, and consists of several orebodies that formed along contacts between Miocene syenogranite, diorite porphyry dykes and late Paleozoic carbonate rocks as discussed by the authors.