L
Lie-Meng Chen
Researcher at Chinese Academy of Sciences
Publications - 47
Citations - 1254
Lie-Meng Chen is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Mafic & Basalt. The author has an hindex of 17, co-authored 39 publications receiving 897 citations. Previous affiliations of Lie-Meng Chen include Ministry of Land and Resources of the People's Republic of China.
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Melting of the subcontinental lithospheric mantle by the Emeishan mantle plume; evidence from the basal alkaline basalts in Dongchuan, Yunnan, Southwestern China
TL;DR: The Emeishan continental flood basalt (ECFB) sequence in Dongchuan, SW China comprises a basal tephrite unit overlain by an upper tholeiitic basalt unit as mentioned in this paper.
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Formation of thick stratiform Fe‐Ti oxide layers in layered intrusion and frequent replenishment of fractionated mafic magma: Evidence from the Panzhihua intrusion, SW China
TL;DR: In this article, the authors proposed that the unusually thick stratiform massive Fe-Ti oxide layers resulted from coupling of gravity settling and sorting of the crystallized Fe- Ti oxides from Fe-Ni-enriched magmas and frequent magma replenishment along the floor of the magma chamber.
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The Giant Xiarihamu Ni-Co Sulfide Deposit in the East Kunlun Orogenic Belt, Northern Tibet Plateau, China
Xie-Yan Song,Jun-Nian Yi,Lie-Meng Chen,Yu-Wei She,Chang-Zheng Liu,Xing-Yan Dang,Qi-An Yang,Shu-Kuan Wu +7 more
TL;DR: The Xiarihamu Ni-Co mine as mentioned in this paper is the largest Ni deposit in China and contains ~157 million metric tons (Mt) sulfide ores with average grades of 0.65 wt % Ni, 0.14 wt% Cu, and 0.013 wt%) Co.
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Syncollisional tholeiitic magmatism induced by asthenosphere upwelling owing to slab detachment at the southern margin of the Central Asian Orogenic Belt
TL;DR: In this article, the authors show that the plume model cannot account for the observed geological characteristics of the Huangshan-Jingerquan mafic-ultramafic belt in the Northern Tianshan.
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Geochemistry of the Huangshandong Ni–Cu deposit in northwestern China: Implications for the formation of magmatic sulfide mineralization in orogenic belts
Yufeng Deng,Yufeng Deng,Xie-Yan Song,Lie-Meng Chen,Taofa Zhou,Franco Pirajno,Franco Pirajno,Feng Yuan,Wei Xie,Dayu Zhang +9 more
TL;DR: The Huangshandong Ni-Cu sulfide deposit as discussed by the authors is located at the southern margin of the Central Asian Orogenic Belt (CAOB) in north Xinjiang, NW China.