GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室
Wang, Christina Yan1,2,3; Bai, Yuying1,2,4; Wei, Bo1,2,3; Minh, Dinh Huu5
Cobaltite-gersdorffite solid solution as a collector of platinum-group elements in the Ban Phuc Ni-Cu-(PGE) sulfide deposit, northern Vietnam
Source PublicationJOURNAL OF ASIAN EARTH SCIENCES
ISSN1367-9120
2023-10-01
Volume255Pages:16
DOI10.1016/j.jseaes.2023.105781
Language英语
WOS Research AreaGeology
AbstractThe Ban Phuc Ni-Cu-(PGE) sulfide deposit in northern Vietnam contains no or few platinum-group minerals (PGM) in massive sulfide ores, and most PGM grains occur in altered disseminated sulfide ores, including sperrylite (PtAs2), irarsite-orarsite-hollingworthite [IrAsS, OsAsS, (Rh,Ir)AsS], and froodite-sobolevskitesudburyite [PdBi2, PdBi, Pd(SbBi) and PdSb]. Discrete PGM grains are enclosed within serpentines and base metal sulfides (BMS) of the disseminated ores. In contrast, small amounts (0.004 vol%) of cobaltite-gersdorffite solid solution (CGss) in massive sulfide ores commonly contain high PGE concentrations relative to the BMS. Textural relationships reveal that the CGss grains crystallize earlier than the host BMS in massive sulfide ores. The CGss grains are found to contain all six PGE and act as the major hosts for the PGE in the massive sulfide ores. The fast Fourier transform (FFT) patterns of high resolution TEM images show that the irarsite (IrAsS) enclosed within the CGss shares the same zone axis of (2 1 2), which results from the exsolution of irarsite from the CGss. On the other hand, the CGss grains without visible PGM show an even distribution of PGE in the crystal and respective FFT patterns of CGss crystals. This is an example of a growing number of cases that massive sulfide ores have been found to contain PGE in As-bearing minerals, either PGM including sperrylite and members of the irarsite-orarsite-hollingworthite solid solution series or CGss. These results argue that PGE in the sulfide melt may enter the CGss at high temperature before the crystallization of monosulfide solution, rather than soluble in BMS, even if the sulfide melt was not As-saturated.
KeywordCobaltite-gersdorffite solid solution (CGss) Platinum-group elements (PGE) Ban Phuc Ni-Cu-(PGE) sulfide deposit Northern Vietnam
WOS IDWOS:001033875000001
Indexed BySCI
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/74584
Collection中国科学院矿物学与成矿学重点实验室
Corresponding AuthorWang, Christina Yan
Affiliation1.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Mineral & Metallogeny, Guangzhou 510640, Peoples R China
2.CAS Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China
3.Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou 510640, Peoples R China
4.Univ Chinese Acad Sci, Beijing, Peoples R China
5.Asian Mineral Resources, Hanoi, Vietnam
Recommended Citation
GB/T 7714
Wang, Christina Yan,Bai, Yuying,Wei, Bo,et al. Cobaltite-gersdorffite solid solution as a collector of platinum-group elements in the Ban Phuc Ni-Cu-(PGE) sulfide deposit, northern Vietnam[J]. JOURNAL OF ASIAN EARTH SCIENCES,2023,255:16.
APA Wang, Christina Yan,Bai, Yuying,Wei, Bo,&Minh, Dinh Huu.(2023).Cobaltite-gersdorffite solid solution as a collector of platinum-group elements in the Ban Phuc Ni-Cu-(PGE) sulfide deposit, northern Vietnam.JOURNAL OF ASIAN EARTH SCIENCES,255,16.
MLA Wang, Christina Yan,et al."Cobaltite-gersdorffite solid solution as a collector of platinum-group elements in the Ban Phuc Ni-Cu-(PGE) sulfide deposit, northern Vietnam".JOURNAL OF ASIAN EARTH SCIENCES 255(2023):16.
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