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Lihui Jia
China University of Geosciences
GeologyMaficGeochemistryZirconPetrogenesis
5Publications
4H-index
41Citations
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Publications 5
Newest
#1Peng Liu (China University of Geosciences)H-Index: 5
#2Jingwen MaoH-Index: 38
Last. Yang LiH-Index: 2
view all 6 authors...
The Lianhuashan deposit has long been regarded as a typical tungsten porphyry deposit, located in the eastern Guangdong Province, in the Southeastern Coastal Metallogenic Belt (SCMB). LA–MC–ICP–MS zircon U–Pb dating of the quartz porphyry yielded a weighted mean 206Pb/238U age of 137.3 ± 2.0 Ma, which is interpreted as the emplacement age of the quartz porphyry. Hydrothermal muscovite yielded a plateau 40Ar/39Ar age of 133.2 ± 0.9 Ma, which is consistent with the zircon U–Pb age, suggesting that...
9 CitationsSource
#1Lihui Jia (China University of Geosciences)H-Index: 4
#2Jingwen Mao (China University of Geosciences)H-Index: 38
Last. Yang LiH-Index: 2
view all 4 authors...
Abstract Comprehensive petrological, zircon U–Pb dating, Hf–O isotopes, whole rock geochemistry and Sr–Nd isotopes data are presented for the Xinwei and Sanrao intrusions in the eastern Guangdong Province, Southeast (SE) China, with an aim to constrain the petrogenesis, tectono-magmatic evolution and evaluate the implication for porphyry Cu–Au–Mo mineralization. The Xinwei intrusion is composed of granodiorite and quartz diorite, whilst the Sanrao intrusion consists of granodiorite. Zircon U–Pb ...
2 CitationsSource
#1Peng Liu (China University of Geosciences)H-Index: 2
#2Jingwen MaoH-Index: 38
Last. Lihui Jia (China University of Geosciences)H-Index: 4
view all 6 authors...
11 CitationsSource
#1Peng Liu (China University of Geosciences)H-Index: 2
#2Jingwen MaoH-Index: 38
Last. Lihui Jia (China University of Geosciences)H-Index: 4
view all 6 authors...
Abstract The Feie'shan greisen–type W–Sn deposit in the eastern Guangdong Province forms part of the Southeastern Coastal Metallogenic Belt (SCMB) in South China. Here we present zircon LA–ICP–MS U–Pb geochronology of the biotite granite which shows a weighted mean 206 Pb/ 238 U age of 134.7 ± 2.0 Ma, consistent with the zircon U–Pb, biotite 40 Ar– 39 Ar and molybdenite Re–Os ages in the previous study. The biotite granite is peraluminous and belongs to high–K calc–alkaline type. It is character...
12 CitationsSource
#1Peng Liu (China University of Geosciences)H-Index: 5
#2Jingwen Mao (China University of Geosciences)H-Index: 38
Last. Hanwen Yang (China University of Geosciences)H-Index: 1
view all 6 authors...
Abstract The Zijinshan intrusion is located to the south of the Tongling ore cluster of the Middle-Lower Yangtze River Valley metallogenic belt (YRB) and even south to the Yangxing–Changzhou Fault (YCF), which separates the YRB and the Jiangnan Massif. It is an I-type high-K calc-alkaline granodiorite with abundant MMEs. Zircon LA-MC-ICP-MS U–Pb ages of 144.0 ± 1.0 Ma and 142.5 ± 1.0 Ma for the host granodiorite and MMEs indicate coeval formation. Biotites from the host granodiorites and MMEs ha...
7 CitationsSource
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