Kai-Xing Wang
Nanjing University
12 Papers
1 Citations
Kai-Xing Wang is an academic researcher from Nanjing University. The author has contributed to research in topics: Zircon & Mafic. The author has an hindex of 6, co-authored 8 publications. Previous affiliations of Kai-Xing Wang include China University of Technology.
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Papers
The geochronological and geochemical constraints on the petrogenesis of the Early Mesozoic A-type granite and diabase in northwestern Fujian province
TL;DR: In this paper, a study of petrography and geochronology reveals that the Dayinchang (DYC hereafter) granitic pluton and Xiamao diabases are Early Mesozoic igneous rocks.
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Chemical composition and Sr isotopes of apatite in the Xiangshan A-type volcanic-intrusive complex, Southeast China: New insight into petrogenesis
Zhi-Qiang Yu,Wei-Feng Chen,Pei-Rong Chen,Kai-Xing Wang,Kai-Xing Wang,Qi-Chun Fang,Xiang-Sheng Tang,Hong-Fei Ling +7 more
TL;DR: In this article, a series of Late Mesozoic A-type granitoids, including the Xiangshan volcanic-intrusive complex, was recently identified along the Gan-Hang volcanic belt, which was close to the boundary of the Yangtze and Cathaysia blocks in South China.
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Magma mingling and chemical diffusion in the Taojiang granitoids in the Hunan Province, China: evidences from petrography, geochronology and geochemistry
TL;DR: Petrographic study and zircon LA-ICP-MS U-Pb dating reveal that the Taojiang pluton is mainly composed of Late Indosinian biotite granodiorites with contemporaneous microgranular enclaves as discussed by the authors.
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Petrogenesis of two Triassic A-type intrusions in the interior of South China and their implications for tectonic transition
TL;DR: A-type granites were derived from partial melting of existing mafic to intermediate rocks in the lower crust in response to the underplating and/or intraplating of mantle-derived magma as discussed by the authors.
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Petrogenesis and geodynamic implications of the Xiema and Ziyunshan plutons in Hunan Province, South China
TL;DR: In this article, Petrographic analysis and zircon LA-ICP-MS dating reveal that the Xiema pluton and the outer portion of the Ziyunshan pluton are composed of Late Triassic (Indosinian) biotite granodiorites and quartz monzonites with contemporaneous mafic microgranular enclaves (hereafter MMEs).
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