In, sn, pb and zn contents and their relationships in ore-forming fluids from some in-rich and in-poor deposits in china
文献类型:期刊论文
作者 | Zhang Qian; Zhu Xiaoqing; He Yuliang; Zhu Zhaohui |
刊名 | Acta geologica sinica-english edition
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出版日期 | 2007-06-01 |
卷号 | 81期号:3页码:450-462 |
关键词 | In-rich deposit In-poor deposit Ore-forming fluid Fluid inclusion Ore-forming elements |
ISSN号 | 1000-9515 |
通讯作者 | Zhang qian(zhqiangeol@163.com) |
英文摘要 | All the indium-rich deposits with indium contents in ores more than 100x10(-6) seems to be of cassiterite-sulfide deposits or sn-bearing pb-zn deposits, e.g., in the dachang sn deposit in guangxi, the dulong sn-zn deposit in yunnan, and the meng'entaolegai ag-pb-zn deposit in inner mongolia, the indium contents in ores range from 98x10(-6) to 236x 10(-6) and show a good positive correlation with contents of zinc and tin, and their correlation coefficients are 0.8781 and 0.7430, respectively. the indium contents from such sn-poor deposits as the fozichong pb-zn deposit in guangxi and the huanren pb-zn deposit in liaoning are generally lower than 10x10(-6), i.e., whether tin is present or not in a deposit implies the enrichment extent of indium in ores. whether the in enrichment itself in the ore -forming fluids or the ore-forming conditions has actually caused the enrichment/depletion of indium in the deposits? after studying the fluid inclusions in quartz crystallized at the main stage of mineralization of several in-rich and in-poor deposits in china, this paper analyzed the contents and studied the variation trend of in, sn, ph and zn in the ore-forming fluids. the results show that the contents of lead and zinc in the ore-forming fluids of in-rich and -poor deposits are at the same level, and the lead contents range from 22x 10(-6) to 81x10(-6) and zinc from 164x10(-6) to 309x10(-6), while the contents of indium and tin in the ore-forming fluids of in-rich deposits are far higher than those of in-poor deposits, with a difference of 1-2 orders of magnitude. indium and tin contents in ore-forming fluid of in-rich deposits are 1.9x10(-6)-4.1x10(-6) and 7x 10-6 -55x10(-6), and there is a very good positive correlation between the two elements, with a correlation coefficient of 0.9552. indium and tin contents in ore-forming fluid of in-poor deposits are 0.03x 10(-6)-0.09x10(-6) and 0.4x10(-6)-2.0x 10(-6), respectively, and there is no apparent correlation between them. this indicates, on one hand, that in-rich oreforming fluids are the material basis for the formation of in-rich deposits, and, on the other hand, tin probably played a very important role in the transport and enrichment of indium. |
WOS关键词 | INDIUM-BEARING ; TIN ; SPHALERITE ; GRANITE ; COPPER ; GEOCHEMISTRY ; GUANGXI ; DACHANG ; ROCKS |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
语种 | 英语 |
WOS记录号 | WOS:000247757800012 |
出版者 | GEOLOGICAL SOC CHINA |
URI标识 | http://www.irgrid.ac.cn/handle/1471x/2380494 |
专题 | 中国科学院大学 |
通讯作者 | Zhang Qian |
作者单位 | 1.Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550002, Guizhou, Peoples R China 2.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China |
推荐引用方式 GB/T 7714 | Zhang Qian,Zhu Xiaoqing,He Yuliang,et al. In, sn, pb and zn contents and their relationships in ore-forming fluids from some in-rich and in-poor deposits in china[J]. Acta geologica sinica-english edition,2007,81(3):450-462. |
APA | Zhang Qian,Zhu Xiaoqing,He Yuliang,&Zhu Zhaohui.(2007).In, sn, pb and zn contents and their relationships in ore-forming fluids from some in-rich and in-poor deposits in china.Acta geologica sinica-english edition,81(3),450-462. |
MLA | Zhang Qian,et al."In, sn, pb and zn contents and their relationships in ore-forming fluids from some in-rich and in-poor deposits in china".Acta geologica sinica-english edition 81.3(2007):450-462. |
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来源:中国科学院大学
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