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Mei-Fu Zhou
University of Hong Kong
386Publications
71H-index
17.2kCitations
Publications 387
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#1Shu-Cheng Tan (Yunnan University)H-Index: 1
#2Jia-Xi Zhou (CAS: Chinese Academy of Sciences)H-Index: 11
Last.Lin Ye (CAS: Chinese Academy of Sciences)H-Index: 7
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Abstract The Upper Yangtze Pb-Zn metallogenic province in South China consists of >400 carbonate-hosted Pb-Zn deposits within Neoproterozoic to Paleozoic strata. Origin of these deposits has been a matter of debate and is thought to be related to Proterozoic basement rocks, Paleozoic sedimentary rocks and the late Permian flood basalts of the Emeishan large igneous province (ELIP). The Tianbaoshan Pb-Zn-(Cu) deposit contains ∼22Mt Pb-Zn ores @ 1.43 wt. % Pb and 10.4 wt. % Zn, and ∼0.1Mt Cu ores ...
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#1Ze-Rui Ray Liu (HKU: University of Hong Kong)
#2Mei-Fu Zhou (HKU: University of Hong Kong)H-Index: 71
Abstract Phosphorite successions in the nearshore Meishucun section and the offshore Gezhongwu section of the Nanhua Basin, South China, were investigated to decipher the circulation pattern of the early Cambrian ocean. The 539–535 Ma phosphorites from the Meishucun section contain authigenic phosphorus-rich mineral aggregates (collophanite grains) with much lower bio-limiting elements, Zn, Cd and Ni, than those from the Gezhongwu section. In contrast, collophanite grains in the 535–526 Ma phosp...
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#1Wei Terry Chen (CAS: Chinese Academy of Sciences)H-Index: 18
#2Mei-Fu Zhou (CAS: Chinese Academy of Sciences)H-Index: 71
Last.YUANHonglin (Northwest University (United States))H-Index: 35
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Precisely dating different generations of mineralization is important for understanding the origin and tectonic environment of ore formation. In this study, we have dated two generations of sulfides from the Lala Fe-Cu deposit, SW China, using in situ Pb-Pb isotopic data obtained by the LA-MC-ICPMS technique. The Lala deposit is composed of Fe-Cu ore bodies hosted in sedimentary-volcanic rocks of the Paleoproterozoic Hekou Group. It has a paragenetic sequence of pre-ore banded pyrite (Stage I) a...
2 CitationsSource
#1Martin Yan Hei Li (HKU: University of Hong Kong)H-Index: 1
#2Mei-Fu Zhou (NU: Nanjing University)H-Index: 71
Last.Anthony E. Williams-Jones (McGill University)H-Index: 46
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1 CitationsSource
#1Wei Wang (Monash University)H-Index: 42
#2Peter A. Cawood (Monash University)H-Index: 70
Last.Jun-Hong ZhaoH-Index: 23
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#1Peng-Fei Zhang (HKU: University of Hong Kong)H-Index: 4
#2Mei-Fu Zhou (HKU: University of Hong Kong)H-Index: 71
Last.Yongsheng He (China University of Geosciences)H-Index: 19
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Abstract Combined Fe isotopic and olivine fabric analyses have been conducted on the nodular chromitites from the Luobusa ophiolite, Tibet, to study the physico-chemical effects of plastic flow in modifying chromitites and their associated mantle peridotites below spreading centers. The Luobusa nodular chromitites are generally composed of fresh dunitic matrices and well-aligned chromite nodules. Olivine grains in both the dunitic matrices and chromite nodules underwent pressure solution, and th...
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#1Peng-Fei Zhang (HKU: University of Hong Kong)H-Index: 4
#2Mei-Fu Zhou (HKU: University of Hong Kong)H-Index: 71
Last.Paul T. Robinson (HKU: University of Hong Kong)H-Index: 14
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#1Xiao-Chun Li (HKU: University of Hong Kong)H-Index: 13
#2Mei-Fu Zhou (HKU: University of Hong Kong)H-Index: 71
Last.Jian-Feng Gao (CAS: Chinese Academy of Sciences)H-Index: 30
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The Khetri Copper Belt (KCB) in northwestern India contains several economically important hydrothermal Cu–(Au) deposits. Orebodies in these deposits are locally rich in monazite-(Ce). In this study, in situ U–Pb ages and Sm–Nd isotopic compositions of monazite-(Ce) are used to constrain the timing of mineralization and to better understand the genesis of the Cu–(Au) deposits. Monazite-(Ce) crystals were identified in the Madhan-Kudhan and Kolihan deposits in the KCB. Most monazite-(Ce) crystals...
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#1Jun-Hong Zhao (China University of Geosciences)H-Index: 23
#2Mei-Fu Zhou (China University of Geosciences)H-Index: 71
Last.Wei Wang (China University of Geosciences)H-Index: 42
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Subduction of oceanic slabs can physically and chemically modify mantle wedges, but how mantle wedges are temporally evolved is difficult to be constrained. In this study, we use in situ zircon U–Pb ages and Hf–O isotopes of mafic intrusions to examine a coupled evolution of magmas and mantle sources above a subduction zone. Neoproterozoic mafic intrusions in the western margin of the Yangtze Block are mostly composed of gabbros that were formed in an arc system during 870–750 Ma followed by gen...
2 CitationsSource
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