华南下寒武统黑色页岩中锌的富集机制
The mechanism of zinc enrichment in the lower Cambrian black shale in South China
查看参考文献55篇
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文摘
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华南大面积下寒武统黑色页岩具有多元素超常富集的显著特征,常被认为与古海洋的氧化还原条件、海洋生产力和热液活动等作用有关。已有成果显示,该区黑色页岩中存在锌(Zn)的富集现象,w(Zn)从几十到上万个10-6。本文通过不同沉积相剖面的元素分布规律、岩相学观测和硫同位素分析研究了锌的来源及其沉淀机制。结果显示:1)华南不同沉积相,甚至同一剖面上存在显著Zn的差异富集(高达15000×10~(-6)),Zn的富集期短暂且峰值出现于520 Ma左右;2)锌主要以细粒或者粗粒分散状的闪锌矿形式产出,与钡冰长石和黄铁矿紧密共生,指示锌的来源与热液有关;3)硫同位素组成变化范围较宽(δ~(34)S = -26.5‰~+44.5‰),暗示着闪锌矿与共生黄铁矿沉淀时有微生物硫酸盐还原作用产生的硫化氢参与。结合埃迪卡拉纪-寒武纪时期海洋的氧化还原分层结构(即表层水体氧化,深部水体缺氧和共存的硫化水体),提出华南下寒武统黑色页岩中Zn的富集是520 Ma左右的热液活动与普遍存在硫化水体相互作用的结果。 |
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其他语种文摘
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The lower Cambrian black shale of South China is characterized with the high concentrations of multi-elements which were proposed to be related to the palaeoceanic redox conditions, marine productivity and hydrothermal activity. Previous research results showed that there is obvious zinc (Zn) enrichment in the black shale in South China with Zn contents widely ranging from hundreds to tens of thousands of ppm. In this paper, the origin and precipitation mechanism of zinc have been studied through the analysis of distribution patterns of Zn in different sedimentary facies sections, petrographic observations, and sulfur isotope analyses. The results are shown below. 1) There are significant differences of enriched Zn (10-15000 ppm) in different lower Cambrian sedimentary facies in South China, or even in different facies of the same section. Especially, the Zn enrichment occurred in a short period with the peak at about 520 Ma; 2) Zn mainly occurred in forms of fine and coarse disseminated sphalerite grains which are closely intergrown with hyalophane and coarse-grained pyrite, indicating that the zinc was sourced from the hydrothermal fluid; 3) The wide range of sulfur isotopic compositions (δ~(34)S values varying from -26.5‰ to +44.5‰) suggested that hydrogen sulfide produced by the microbial sulfate reduction was involved in the precipitation of sphalerite and intergrown pyrite. Combined with the knowledge of stratified structure of the redox for the palaeocean in the Ediacaran-Cambrian transition period, namely, the overlying oxic surface water, the anoxic deep water, and the accompanied mid-depth sulfidic water (e.g., euxinia), it is proposed that the Zn enrichment in the lower Cambrian black shale in South China was resulted from the interaction of hydrothermal fluid and commonly existed sulfidic water at about 520 Ma. |
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来源
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矿物学报
,2023,43(4):481-489 【核心库】
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DOI
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10.16461/j.cnki.1000-4734.2023.43.029
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关键词
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牛蹄塘组
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留茶坡组
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热液
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铅锌矿床
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钡冰长石
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地址
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中国科学院地球化学研究所, 矿床地球化学国家重点实验室, 贵州, 贵阳, 550081
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中国科学院大学, 北京, 100049
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贵州省地质矿产勘查开发局一0一地质大队, 贵州, 凯里, 556000
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贵州省地质矿产勘查开发局贵州省地质调查院, 贵州, 贵阳, 550081
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语种
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中文 |
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文献类型
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研究性论文 |
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ISSN
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1000-4734 |
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学科
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地质学 |
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基金
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贵州省高层次人才创新创业择优资助项目
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中国科学院西部之光人才培养计划
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国家自然科学基金
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文献收藏号
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CSCD:7500617
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参考文献 共
55
共3页
|
|
1.
范德廉.
中国的黑色岩系及其有关矿床,2004:1-6
|
被引
45
次
|
|
|
|
|
2.
Tribovillard N. Trace metals as paleoredox and paleoproductivity proxies: an update.
Chem Geol,2006,232:12-32
|
被引
491
次
|
|
|
|
|
3.
Li C. A stratified redox model for the Ediacaran ocean.
Science,2010,328:80-83
|
被引
98
次
|
|
|
|
|
4.
Tribovillard N. Analysis of marine environmental conditions based on molybdenum-uranium covariation-applications to Mesozoic paleoceanography.
Chem Geol,2012,324/325:46-58
|
被引
77
次
|
|
|
|
|
5.
Sahoo S K. Ocean oxygenation in the wake of the Marinoan glaciation.
Nature,2012,489:546-549
|
被引
60
次
|
|
|
|
|
6.
Leach D L. Sediment-hosted lead-zinc deposits in Earth history.
Econ Geol,2010,105(3):593-625
|
被引
108
次
|
|
|
|
|
7.
Kelley K D. Textural, compositional, and sulfur isotope variations of sulfide minerals in the Red Dog Zn-Pb-Ag deposits, Brooks Range, Alaska: implications for ore formation.
Econ Geol,2004,99:1509-1532
|
被引
26
次
|
|
|
|
|
8.
Magnall J M. A new subseafloor replacement model for the Macmillan Pass clastic-dominant Zn-Pb±Ba deposits (Yukon, Canada).
Econ Geol,2020,115(5):953-959
|
被引
1
次
|
|
|
|
|
9.
Canfield D E. The early history of atmospheric oxygen: homage to Robert M. Garrels.
Annu Rev Earth Planet Sci,2005,33(1):1-36
|
被引
72
次
|
|
|
|
|
10.
Zhu M. From Snowball Earth to the Cambrian bioradiation: calibration of Ediacaran-Cambrian earth history in South China.
Palaeogeogr Palaeoclimatol Palaeoecol,2007,254(1):1-6
|
被引
10
次
|
|
|
|
|
11.
Lyons T W. The rise of oxygen in Earth's early ocean and atmosphere.
Nature,2014,506:306-315
|
被引
1
次
|
|
|
|
|
12.
Wen H. Reconstruction of early Cambrian ocean chemistry from Mo isotopes.
Geochim Cosmochim Acta,2015,164:1-16
|
被引
9
次
|
|
|
|
|
13.
Chen X. Rise to modern levels of ocean oxygenation coincided with the Cambrian radiation of animals.
Nat Commun,2015,6:7142
|
被引
43
次
|
|
|
|
|
14.
Lehmann B. Highly metalliferous carbonaceous shale and Early Cambrian seawater.
Geology,2007,35(5):403-406
|
被引
62
次
|
|
|
|
|
15.
Xu L G. Seawater contribution to polymetallic Ni-Mo-PGE-Au mineralization in Early Cambrian black shales of South China: Evidence from Mo isotope, PGE, trace element, and REE geochemistry.
Ore Geol Rev,2013,52:66-84
|
被引
26
次
|
|
|
|
|
16.
Liu Z. Early Cambrian ocean mixing recorded by phosphorite successions in the Nanhua Basin, South China.
Precambrian Res,2020,349:105414
|
被引
1
次
|
|
|
|
|
17.
Lu Z. Control of V accumulation in organic-rich shales by clay-organic nanocomposites.
Chem Geol,2021,567:120100
|
被引
1
次
|
|
|
|
|
18.
Guo Q J. Trace element chemostratigraphy of two Ediacaran-Cambrian successions in South China: implications for organosedimentary metal enrichment and silicification.
Palaeogeogr Palaeoclimatol Palaeoecol,2007,254:194-216
|
被引
61
次
|
|
|
|
|
19.
Feng L. A sulfate control on marine mid-depth euxinia on the early Cambrian (ca. 529-521 Ma) Yangtze platform, South China.
Precambrian Res,2014,246:123-133
|
被引
15
次
|
|
|
|
|
20.
李超. 寒武纪早期大气-海洋氧含量与生命大爆发.
矿物岩石地球化学通报,2015,34(3):501-508
|
被引
7
次
|
|
|
|
|
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