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DOI | 10.1180/mgm.2023.41 |
Tennantite-(Ni), Cu6(Cu4Ni2)As4S13, from Luobusa ophiolite, Tibet, China: a new Ni member of the tetrahedrite group | |
Wang, Yanjuan; Chen, Rujun; Gu, Xiangping; Hou, Zengqian; Nestola, Fabrizio; Yang, Zhusen; Fan, Guang; Dong, Guochen; Ye, Lijuan; Qu, Kai | |
发表日期 | 2023 |
ISSN | 0026-461X |
EISSN | 1471-8022 |
起始页码 | 591 |
结束页码 | 598 |
卷号 | 87期号:4 |
英文摘要 | The new mineral tennantite-(Ni), Cu-6(Cu4Ni2)As4S13, has been discovered from the Luobusa Chromitite, Tibet, southwestern China. Tennantite-(Ni) occurs as anhedral grains ranging from 2 to 20 mu m in size. In reflected light microscopy, tennantite-(Ni) is isotropic and appears yellow-greenish grey. Reflectance data for Commission on Ore Mineralogy wavelengths in air for tennantite-(Ni) are: 31.0 (470 nm), 29.6 (546 nm), 29.6 (589 nm) and 29.3 (650 nm). Electron microprobe analysis for holotype material gave the empirical formula (on basis of total cations = 16 apfu): Cu-M(2)(6) (M(1))[Cu-4.00(Ni0.97Cu0.53Fe0.50)Sigma(2.00)vertical bar Sigma(X(3))(6.00)(As2.94Sb1.06)Sigma S-4(12.77). Tennantite-(Ni) is cubic, with space group I (4) over bar 3m (#217), a =10.2957(9) angstrom, V = 1091.4(3) angstrom(3) and Z = 2. By using single-crystal X-ray diffraction, the crystal structure has been determined and refined to a final R-1 = 0.0423 on the basis of 163 independent reflections [F-o > 4 sigma (F-o)]. The calculated seven strongest powder X-ray diffraction lines [d in angstrom (I) (hkl)] are: 2.972 (100) (222), 1.820 (83) (440), 2.574 (28) (400), 1.552 (18) (622), 3.640 (10) (220), 1.880 (10) (521) and 1.287 (7) (800). Tennantite-(Ni) is isostructural with other tetrahedrite-group minerals, and nickel is hosted at the tetrahedrally coordinated M(1) site, along with Cu and minor Fe. The mineral and its name have been approved by the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association (IMA2021-018). |
关键词 | tennantite-(Ni)new mineraltetrahedrite groupsulfosaltcrystal structureLuobusa chromitite deposit |
英文关键词 | CRYSTAL-STRUCTURE; REFINEMENT; STABILITY; BINNITE |
WOS研究方向 | Mineralogy |
WOS记录号 | WOS:001038418100001 |
来源期刊 | MINERALOGICAL MAGAZINE |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/283252 |
作者单位 | China University of Geosciences - Beijing; Central South University; China Geological Survey; Chinese Academy of Geological Sciences; Institute of Geology, Chinese Academy of Geological Sciences; University of Padua; China Geological Survey; Chinese Academy of Geological Sciences; China Geological Survey; Tianjin Center, China Geological Survey; Nanjing University |
推荐引用方式 GB/T 7714 | Wang, Yanjuan,Chen, Rujun,Gu, Xiangping,et al. Tennantite-(Ni), Cu6(Cu4Ni2)As4S13, from Luobusa ophiolite, Tibet, China: a new Ni member of the tetrahedrite group[J],2023,87(4). |
APA | Wang, Yanjuan.,Chen, Rujun.,Gu, Xiangping.,Hou, Zengqian.,Nestola, Fabrizio.,...&Qu, Kai.(2023).Tennantite-(Ni), Cu6(Cu4Ni2)As4S13, from Luobusa ophiolite, Tibet, China: a new Ni member of the tetrahedrite group.MINERALOGICAL MAGAZINE,87(4). |
MLA | Wang, Yanjuan,et al."Tennantite-(Ni), Cu6(Cu4Ni2)As4S13, from Luobusa ophiolite, Tibet, China: a new Ni member of the tetrahedrite group".MINERALOGICAL MAGAZINE 87.4(2023). |
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