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Mei-Fu Zhou
Chinese Academy of Sciences
380Publications
69H-index
15.8kCitations
Publications 380
Newest
Published on 2019in Precambrian Research3.83
Ze-Rui Ray Liu (HKU: University of Hong Kong), Mei-Fu Zhou69
Estimated H-index: 69
(HKU: University of Hong Kong)
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...
Published on Jun 1, 2019in Mineralium Deposita3.40
Wei Terry Chen17
Estimated H-index: 17
(CAS: Chinese Academy of Sciences),
Mei-Fu Zhou69
Estimated H-index: 69
(CAS: Chinese Academy of Sciences)
+ 3 AuthorsHonglin Yuan1
Estimated H-index: 1
(Northwest University (United States))
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...
Published on May 1, 2019in Economic Geology3.29
Martin Yan Hei Li (HKU: University of Hong Kong), Mei-Fu Zhou69
Estimated H-index: 69
(NU: Nanjing University),
Anthony E. Williams-Jones43
Estimated H-index: 43
(McGill University)
Published on May 1, 2019in Acta Geologica Sinica-english Edition
Wei Wang (Monash University), Peter A. Cawood66
Estimated H-index: 66
(Monash University)
+ 3 AuthorsJun-Hong Zhao24
Estimated H-index: 24
Published on May 1, 2019in Geochimica et Cosmochimica Acta4.26
Peng-Fei Zhang4
Estimated H-index: 4
(HKU: University of Hong Kong),
Mei-Fu Zhou69
Estimated H-index: 69
(HKU: University of Hong Kong)
+ 3 AuthorsYongsheng He14
Estimated H-index: 14
(China University of Geosciences)
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...
Published on May 1, 2019in Acta Geologica Sinica-english Edition
Peng-Fei Zhang4
Estimated H-index: 4
(HKU: University of Hong Kong),
Mei-Fu Zhou69
Estimated H-index: 69
(HKU: University of Hong Kong)
+ 1 AuthorsPaul T. Robinson13
Estimated H-index: 13
(HKU: University of Hong Kong)
Published on Apr 1, 2019in Mineralium Deposita3.40
Xiao-Chun Li7
Estimated H-index: 7
(HKU: University of Hong Kong),
Mei-Fu Zhou69
Estimated H-index: 69
(HKU: University of Hong Kong)
+ 2 AuthorsJian-Feng Gao27
Estimated H-index: 27
(CAS: Chinese Academy of Sciences)
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...
Published on Apr 1, 2019in Contributions to Mineralogy and Petrology3.23
Jun-Hong Zhao24
Estimated H-index: 24
(China University of Geosciences),
Mei-Fu Zhou69
Estimated H-index: 69
(China University of Geosciences)
+ 2 AuthorsWei Wang (China University of Geosciences)
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...
Published on Mar 1, 2019in Geological Society of America Bulletin3.97
Wei Wang43
Estimated H-index: 43
(Monash University),
Wei Wang (Monash University)+ 2 AuthorsJun-Hong Zhao24
Estimated H-index: 24
(China University of Geosciences)
Published on Feb 1, 2019in Chemical Geology3.62
Ze-Rui Ray Liu (HKU: University of Hong Kong), Mei-Fu Zhou69
Estimated H-index: 69
(China University of Geosciences)
+ 2 AuthorsJian-Feng Gao27
Estimated H-index: 27
(CAS: Chinese Academy of Sciences)
Abstract Titanium (Ti) is typically hosted in detrital minerals in marine sediments and has long been considered to be immobile during diagenesis. In this study, the authigenic titania minerals, brookite and anatase, are observed in early Cambrian carbonaceous shales from the Meishucun and Zhajin sections of South China, respectively. Black shales in the Meishucun section have total organic carbon (TOC) contents from 1.6 to 3.9 wt% and HI (hydrogen index) values from 3.8 to 20 mg HC/g TOC, where...
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