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Geochemistry of pyrite from stratabound massive sulfide deposits, Tongling region, China: Implication for their genesis | |
Xie, Jiancheng1; Ge, Likai1; Fang, De1; Li, Quanzhong1; Qian, Lin1; Li, Zhensheng1; Yan, Jun1; Sun, Weidong2,3,4![]() | |
2020-05-01 | |
Source Publication | ORE GEOLOGY REVIEWS
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ISSN | 0169-1368 |
Volume | 120Pages:16 |
Corresponding Author | Xie, Jiancheng(xiejiancheng08@hfut.edu.cn) |
Abstract | Stratabound massive sulfide deposits are widely distributed along Middle-Lower Yangtze River metallogenic belt, in eastern China. There has much debate as to whether these deposits were associated with Late Mesozoic igneous or Carboniferous sedimentary exhalative (SEDEX). Three-type pyrites, i.e., colloform (Py1), fine-grained (Py2) and medium- to coarse-grained (Py3), from Xinqiao and Taoyuan stratabound massive sulfide deposits in Tongling region were investigated using electron probe microanalysis (EPMA), in-situ laser-ablation inductivelycoupled plasma-mass spectrometry (LA-ICP-MS) and sulfur isotopic analysis. The analytic data indicate that the three-type pyrites have high S and As, and relatively consistent Au contents. The Au, Ag, Bi, Sb and Pb elements are mainly of lattice bound appearance in the Xinqiao and Taoyuan pyrites. Low Au (mainly < 5 ppm) and Ni (commonly < 10 ppm) contents, high Co/Ni (mainly > 1), Se/Tl (mainly > 1) and delta S-34(CDT) (4.0 parts per thousand to 5.9 parts per thousand) values of the studied Xinqiao and Taoyuan pyrites imply a magmatic-hydrothermal origin. High Bi (> 1 ppm) and Mo contents, and low Co/Ni ratios (< 0.1) of the studied Xinqiao and Taoyuan pyrites reflect a sedimentary contribution to the magmatic-hydrothermal system. Combined with previous results, the Xinqiao stratabound mineralization is most likely to be genetically with the magmatic-hydrothermal fluids by the addition of a sedimentary component. |
Keyword | In situ geochemistry S isotope Pyrite Stratabound massive sulfide deposit Tongling region |
DOI | 10.1016/j.oregeorev.2020.103430 |
Indexed By | SCI |
Language | 英语 |
Funding Project | National Natural Science Foundation of China[41373045] ; National Key R&D Program of China[2016YFC0600404] |
WOS Research Area | Geology ; Mineralogy ; Mining & Mineral Processing |
WOS Subject | Geology ; Mineralogy ; Mining & Mineral Processing |
WOS ID | WOS:000530673300049 |
Publisher | ELSEVIER |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.qdio.ac.cn/handle/337002/167452 |
Collection | 深海极端环境与生命过程研究中心 |
Corresponding Author | Xie, Jiancheng |
Affiliation | 1.Hefei Univ Technol, Sch Resources & Environm Engn, Hefei 230009, Peoples R China 2.Chinese Acad Sci, Ctr Deep Sea Res, Inst Oceanol, Qingdao 266071, Peoples R China 3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China 4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
Recommended Citation GB/T 7714 | Xie, Jiancheng,Ge, Likai,Fang, De,et al. Geochemistry of pyrite from stratabound massive sulfide deposits, Tongling region, China: Implication for their genesis[J]. ORE GEOLOGY REVIEWS,2020,120:16. |
APA | Xie, Jiancheng.,Ge, Likai.,Fang, De.,Li, Quanzhong.,Qian, Lin.,...&Sun, Weidong.(2020).Geochemistry of pyrite from stratabound massive sulfide deposits, Tongling region, China: Implication for their genesis.ORE GEOLOGY REVIEWS,120,16. |
MLA | Xie, Jiancheng,et al."Geochemistry of pyrite from stratabound massive sulfide deposits, Tongling region, China: Implication for their genesis".ORE GEOLOGY REVIEWS 120(2020):16. |
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