中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Laser Ablation-Inductively Coupled Plasma Mass Spectrometry (LA-ICPMS) elemental mapping and its applications in ore geology

文献类型:期刊论文

作者Zhou LingLi4,5,6,7; Zeng QingDong4,5,6; Sun GuoTao4,5,6; Duan XiaoXia3; bonnetti, Christophe2; Riegler, Thomas7; Long, Darrel G. F.1; Kamber, Balz7
刊名ACTA PETROLOGICA SINICA
出版日期2019
卷号35期号:7页码:1964-1978
关键词LA-ICPMS Elemental mapping Pyrite Qingchenzi Pb-Zn deposit Bayinwula U deposit Pardo placer Au deposit
ISSN号1000-0569
DOI10.18654/1000-0569/2019.07.02
英文摘要With the development of two-dimensional trace element mapping by laser-ablation inductively-coupled-plasma mass spectrometry (LA-ICP-MS), it is now possible to reveal in much greater detail any compositional interior textures of the pyrites, thus permitting the investigation of the history of pyrite crystals and providing new insight into the genesis and evolution of mineralisation. Exploiting the advantages of high spatial resolution, low detection limits, and capability of full quantification, LA-ICP-MS elemental mapping is being widely applied to imaging sulphides from various types of deposits. In this study, we applied the LA-ICP-MS elemental mapping technique on pyrites from different types of deposits from China and Canada, for the purpose of monitoring the changes of physio-chemical condition, defining ore genesis, and revealing the distribution patterns of precious metals. The interior compositional textures of pyrites show that the mineralization system of the Bayinwula roll-front U deposit in Inner Mongolia was open and continuously affected by the re-charge of oxidized groundwater, along with a periodic change of pH and Eh that affected the activities of sulphate bacteria and the associated U mineralization. The trace element maps of pyrites from the Zhenzigou Pb-Zn deposit in Liaoning Province indicate that several episodes of fluids were involved and responsible for the mineralisation, namely, an early stage of syn-sedimentary origin and a late hydrothermal mineralisation related to the Yanshanian magmatic activity. The trace element distribution patterns of pyrites from the Palaeoproterozoic placer Au deposit in Canada showed that the subeuhedral-euhedral pyrite, which is a dominant type of pyrite in the conglomerates, is detrital origin and later modified by hydrothermal (or metamorphic) fluids, and Au is mostly associated with the detrital pyrite grains/cores, and disseminated in the porosity on the surface.
WOS关键词TRACE-ELEMENT ; MINOR ELEMENTS ; PYRITE ; DEPOSIT ; GOLD ; GENESIS ; SULFUR ; TOWNSHIPS ; MINERALS ; CLEMENT
WOS研究方向Geology
语种英语
WOS记录号WOS:000491151100002
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/93890]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Zhou LingLi
作者单位1.Laurentian Univ, Dept Earth Sci, Sudbury, ON P3E 2C6, Canada
2.East China Univ Technol, State Key Kaboratory Kuclear Resources & Environm, Nanchang 330013, Jiangxi, Peoples R China
3.Hefei Univ Technol, Sch Resources & Environm Engn, Hefei 230009, Anhui, Peoples R China
4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
5.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
7.Trinity Coll Dublin, Sch Nat Sci, Dept Geol, iCRAG, Dublin 2, Ireland
推荐引用方式
GB/T 7714
Zhou LingLi,Zeng QingDong,Sun GuoTao,et al. Laser Ablation-Inductively Coupled Plasma Mass Spectrometry (LA-ICPMS) elemental mapping and its applications in ore geology[J]. ACTA PETROLOGICA SINICA,2019,35(7):1964-1978.
APA Zhou LingLi.,Zeng QingDong.,Sun GuoTao.,Duan XiaoXia.,bonnetti, Christophe.,...&Kamber, Balz.(2019).Laser Ablation-Inductively Coupled Plasma Mass Spectrometry (LA-ICPMS) elemental mapping and its applications in ore geology.ACTA PETROLOGICA SINICA,35(7),1964-1978.
MLA Zhou LingLi,et al."Laser Ablation-Inductively Coupled Plasma Mass Spectrometry (LA-ICPMS) elemental mapping and its applications in ore geology".ACTA PETROLOGICA SINICA 35.7(2019):1964-1978.

入库方式: OAI收割

来源:地质与地球物理研究所

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