H
Hong-Rui Fan
Researcher at Chinese Academy of Sciences
Publications - 155
Citations - 5287
Hong-Rui Fan is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Pyrite & Zircon. The author has an hindex of 36, co-authored 127 publications receiving 3962 citations.
Papers
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Petrogenesis of post-orogenic syenites in the Sulu Orogenic Belt, East China: geochronological, geochemical and Nd-Sr isotopic evidence
TL;DR: The Jiazishan metamorphic orogenic complex is composed of potassic to ultrapotassic pyroxene syenite and associated mafic dikes.
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Decratonic gold deposits
TL;DR: In this paper, the authors present a summary and discussion on time-space distribution and ore genesis of gold deposits in the North China craton (NCC) in the context of the timing, spatial variation, and decratonic processes.
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Ore-forming fluids associated with granite-hosted gold mineralization at the Sanshandao deposit, Jiaodong gold province, China
TL;DR: The Sanshandao gold deposit as mentioned in this paper is a typical highly fractured and altered, disseminated gold system with high-grade, quartz-sulphide vein/veinlet stockworks that cut Mesozoic granodiorite.
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Reactivation of the Archean lower crust: Implications for zircon geochronology, elemental and Sr-Nd-Hf isotopic geochemistry of late Mesozoic granitoids from northwestern Jiaodong Terrane, the North China Craton
Kui-Feng Yang,Hong-Rui Fan,M. Santosh,M. Santosh,Fang-Fang Hu,Simon A. Wilde,Ting-Guang Lan,Li-Na Lu,Yongsheng Liu +8 more
TL;DR: The late Mesozoic granitoids widely distributed in the northwestern Jiaodong Terrane are important markers of cratonic destruction and lithospheric thinning of the eastern North China Craton.
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Mesoproterozoic carbonatitic magmatism in the Bayan Obo deposit, Inner Mongolia, North China: Constraints for the mechanism of super accumulation of rare earth elements
TL;DR: In this paper, the authors show that three types of carbonatite dykes occur around the Bayan Obo mine in North China, including dolomite, calcite and calcite-dolomitic carbonatites.