L
Lian-Xun Wang
Researcher at China University of Geosciences (Wuhan)
Publications - 45
Citations - 747
Lian-Xun Wang 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 12, co-authored 36 publications receiving 487 citations. Previous affiliations of Lian-Xun Wang include University of Tübingen & Leibniz University of Hanover.
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Genesis of leucogranite by prolonged fractional crystallization: A case study of the Mufushan complex, South China
TL;DR: In this article, major and trace elemental geochemical data, Sr-Nd-Hf isotopes and zircon U-Pb ages for igneous rocks of the Mufushan complex were presented.
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Discovery of Paleoproterozoic rapakivi granite on the northern margin of the Yangtze block and its geological significance
TL;DR: Huashanguan rapakivi granites were characterized as having high values of Si, K, Fe, Th, U, La, Ga, Ce, Sm and LREE, low values of Ca, Mg, Sr, Nb, Y and HREE.
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Halogen geochemistry of I- and A-type granites from Jiuhuashan region (South China): Insights into the elevated fluorine in A-type granite
TL;DR: In this paper, the A-type and I-type granites and mafic dyke rocks from the Jiuhuashan region (South China) have been geochemically studied with a special emphasis on their halogen (F, Cl, Br, I) contents to better understand the role of halogens during their genesis.
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Apatites from the Kaiserstuhl Volcanic Complex, Germany: new constraints on the relationship between carbonatite and associated silicate rocks
Lian-Xun Wang,Lian-Xun Wang,Michael A.W. Marks,Thomas Wenzel,Anette von der Handt,Jörg Keller,Holger Teiber,Gregor Markl +7 more
TL;DR: Apatites from carbonatites, related alkaline silicate rocks, a carbonate-bearing melilititic dyke dyke rock (bergalite), and a diatreme breccia (containing both carbonate and silicate fragments) of the Miocene Kaiserstuhl Volcanic Complex, SW Germany, are used to reconstruct the petrogenetic relationship among these rocks as discussed by the authors.
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Petrogenesis and tectonic implications of Upper Triassic appinite dykes in the East Kunlun orogenic belt, northern Tibetan Plateau
Bin Liu,Bin Liu,Changqian Ma,Jian Huang,Jian Huang,Lian-Xun Wang,Shao-Qing Zhao,Rong Yan,Yang Sun,Fu-Hao Xiong +9 more
TL;DR: In this paper, the authors presented geochronological, mineralogical, geochemical, and Sr-Nd isotopic data for recently identified Upper Triassic appinite dyke swarms in the East Kunlun orogenic belt (EKOB), northern Tibetan Plateau Zircon U-Pb isotopic analyses using SHRIMP and LA-ICP-MS techniques yield 206 Pb/ 238 U ages of 2261-±-19-Ma and 2264-±−35-Ma, which can be interpreted as the crystallization ages of