地球科学进展

地球科学进展 ›› 2019, Vol. 34 ›› Issue (4): 382 -398. doi: 10.11867/j.issn.1001-8166.2019.04.0382

固体地球科学 上一篇    下一篇

金川超大型 Ni-Cu-( PGE)矿床橄榄石微量元素特征及地质意义
康健 1, 2( ),陈列锰 1( ),宋谢炎 1,戴智慧 1,郑文勤 1   
  1. 1. 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
    2. 中国科学院大学，北京 100049
  • 收稿日期:2018-12-25 修回日期:2019-02-03 出版日期:2019-04-10
  • 通讯作者: 陈列锰 E-mail:kaingjian@mail.gyig.ac.cn;chenliemeng@vip.gyig.ac.cn
  • 基金资助:
    国家重点研发计划项目“典型成矿系统演化规律与时空自相似结构”(编号：2016YFC0600503);国家自然科学基金面上项目“Mg-Fe同位素对东昆仑造山带夏日哈木和石头坑德含铜镍硫化物岩体源区的制约”(编号：41873026)

Trace Elements in Olivines from the Giant Jinchuan Ni-Cu-( PGE) Deposit, NW China, and Its Geological Implication

Jian Kang 1, 2( ),Liemeng Chen 1( ),Xieyan Song 1,Zhihui Dai 1,Wenqin Zheng 1   

  1. 1. State Key Laboratory of Ore Deposit Geochemistry, Institude of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
    2. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2018-12-25 Revised:2019-02-03 Online:2019-04-10 Published:2019-05-27
  • Contact: Liemeng Chen E-mail:kaingjian@mail.gyig.ac.cn;chenliemeng@vip.gyig.ac.cn
  • About author: Kang Jian （1994-）， male， Tianshui City， Gansu Province， Master student. Research areas include magma sulfide deposits. E-mail: kaingjian@mail.gyig.ac.cn | Kang Jian （1994-）， male， Tianshui City， Gansu Province， Master student. Research areas include magma sulfide deposits. E-mail: kaingjian@mail.gyig.ac.cn
  • Supported by:
    Project supported by the National Key Research and Development Program "The evolution law of typical metallogenic system and its spatio-temporal self-similar structure"(No.2016YFC0600503);The National Natural Science Foundation of China "Restriction of Mg-Fe isotope on source area of Ni-Cu sulfide deposits in Xiarihamu and Shitoukengde in east Kunlun orogenic belt"(No.41873026)
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我国金川超大型铜镍硫化物矿床是世界上第三大在采岩浆硫化物矿床，Ni开采量仅次于俄罗斯Noril’sk-Talnakh和加拿大Sudbury矿床，其成因研究备受关注。利用激光—等离子体质谱（LA-ICP-MS）原位分析了金川岩体中橄榄石微量元素含量，并探讨了影响元素含量变化的因素，进而阐述成岩及成矿过程。分析结果显示橄榄石中元素Ni，Cr与Fo呈负相关，Mn/Fe与Fo呈正相关，而Mn/Zn，Zn/Fe与Fo无相关性。在原始地幔橄榄石多元素标准化图中，金川Ⅰ号和Ⅱ号岩体橄榄石具相同的配分模式，均显示Cr，V，Ni，Co和Ti的亏损，富集不相容元素Zr，Y，Ti，Sc和Ca的特征。元素变化特征暗示Ⅰ号和Ⅱ号岩体具相同的母岩浆成分；与铬尖晶石的共结使橄榄石亏损Cr，V和Ti元素，而熔离的硫化物及其与橄榄石的相互反应共同影响着橄榄石中Ni和Co元素的含量。Ⅱ号岩体橄榄石较Ⅰ号岩体具较低的Cr和V含量，暗示Ⅱ号岩体母岩浆较Ⅰ号岩体经历了更高程度的演化。橄榄石高的Mn/Zn值（>13）和低的Zn/Fe值（<11）指示金川岩体岩浆可能起源于橄榄岩地幔的部分熔融，而非辉石岩地幔源区。

关键词: 橄榄石, 微量元素, 岩浆演化, 金川岩体

The giant Jinchuan magmatic sulfide deposit in China is the third largest mining deposits in the world. Although many research have been done, there still exist some debates in the genesis of deposit. This study using the LA-IC-MS to obtain the trace elements concentrations of the olivine in order to discuss the mechanism of influence the element variability and illustrate the process of magmatism and ore-forming. The analytical results show that Ni, Co correlate negatively with Fo in the olivine, Mn/Fe is positively correlate with Fo, while Mn/Zn and Zn/Fe show no obvious correlation with Fo. The primitive mantle olivine-normalized trace element patterns of the Jinchuan olivine show that Jinchuan Ⅰ, Ⅱ intrusions have the same trace elements characteristics, which display negative Cr, V, Ni, Co and Ti anomalies and enrichment of Zr, Y, Ti, Sc and Ca. The multi-element patterns of the Jinchuan olivine imply same parental magma in the intrusion Ⅰ and Ⅱ. The spinel which cocrystallization with the olivine make it display negative Cr, V and Ti anomalies. The contents of Ni and Co in olivine are influenced by the process of sulfide segregation and the reaction between sulfide and olivine. The lower content of Cr and V in olivine of the intrusion Ⅱ compared with the intrusion Ⅰ imply that the parental magma of the intrusion Ⅱ was more evolved. Higher Mn/Zn (>13) ratios and lower Zn/Fe (<11) ratios indicate that the magma of Jinchuan intrusion likely originate from partial melting of peridotite mantle possibly, instead of pyroxene mantle sources.

Key words: Olivine, Trace elements, Magmatic evolution, Jinchuan instrusion.

中图分类号: 

图1 龙首山地体和金川岩体地质简图
Fig.1 Geological maps of the Longshou Terrain and the Jinchuan intrusion
图2 金川岩体不同岩相中橄榄石及硫化物结构
Fig.2 Olivine and sulfide textures of the Jinchuan intrusion in different petrofacies
表1 金川岩体橄榄石主、微量元素分析结果
Table 1 The major and trace elements of olivine in Jinchuan intrusion
采样位置 I号岩体下部岩相带
样号 JC06-233 JC13-106 JC13-102 JC13-101 JC13-107 JC13-230
岩性 粗粒硫化物橄榄岩 粗粒二辉橄榄岩 粗粒硫化物二辉橄榄岩 粗粒斜长二辉橄榄岩 粗粒二辉橄榄岩 粗粒二辉橄榄岩
点号 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-4 Ol-1 Ol-2 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2
主量元素质量百分含量/% MgO 43.4 43.3 43.6 42.1 42.9 42.3 43.7 41.5 42.1 42.7 42.0 42.9 41.6 41.6 42.3 41.9 41.0
Al2O3 0.0 0.0 0.0 0.1 0.0 0.0 0.1 0.0 0.1 0.1 0.0 0.0 0.0 0.0 0.0 0.0 0.0
SiO2 40.2 41.0 40.5 40.0 40.3 40.0 40.1 39.7 39.3 39.1 39.8 40.2 39.7 39.5 39.6 39.1 39.5
CaO 0.1 0.1 0.1 0.5 0.1 0.0 0.1 0.1 0.2 0.0 0.1 0.0 0.1 0.2 0.1 0.0 0.0
TiO2 0.0 0.0 0.1 0.0 0.0 0.1 0.0 0.1 0.1 0.0 0.0 0.0 0.0 0.0 0.1 0.0 0.0
Cr2O3 0.0 0.1 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
MnO 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.3 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2
FeO 15.0 14.9 15.0 15.1 15.8 16.0 15.8 17.4 17.2 17.2 17.2 16.5 17.6 16.8 16.6 17.9 17.1
Na2O 0.0 0.0 0.0 0.1 0.1 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
K2O 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
NiO 0.2 0.2 0.2 0.2 0.2 0.3 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2
总量 99.1 99.8 99.7 98.3 99.6 98.9 100.3 99.2 99.4 99.6 99.7 100.1 99.2 98.6 98.9 99.0 98.0
Fo 83.7 83.9 83.8 83.3 82.9 82.5 83.2 81.0 81.3 81.5 81.3 82.2 80.8 81.5 82.0 80.7 81.1
微量元素/(μg/g) Li 6.62 3.97 3.73 3.25 3.17 3.79 5.01 6.40 5.88 2.26 4.18 2.94 3.38 6.58 6.26 7.27 5.02
Na 47.8 25.2 17.4 15.5 13.8 15.2 20.0 16.9 55.1 7.1 5.3 34.8 20.2 19.4 5.4 112.0 22.3
Al 60.7 95.2 118.4 140.6 70.6 70.0 119.5 129.9 108.1 186.0 121.7 320.0 97.8 109.5 70.1 98.4 92.3
P 68.6 58.7 41.5 44.1 47.0 41.0 54.8 79.7 66.6 48.4 80.7 66.1 45.2 63.2 61.8 86.3 49.9
Ca 586.0 792 950 1308 609 602 733 1154 858 324 465 1550 821 523 263 137 56.0
Sc 8.50 5.99 3.99 4.26 4.92 4.12 4.53 4.66 3.97 3.56 4.16 5.64 3.86 3.48 3.92 1.54 1.51
Ti 151. 108 122 59 137 153 78.9 59.3 59.9 47.3 35.9 40.4 86.5 106 113 119 130
V 6.64 4.28 5.64 5.06 3.87 3.99 5.60 5.95 4.67 5.29 2.15 11.5 4.90 4.08 3.70 1.30 1.19
Cr 145.0 138.3 135.1 122.1 71.4 97.5 116.9 89.7 82.5 94.7 95.2 161.7 80.8 61.8 34.9 83.4 76.5
Mn 1 882 1 844 1 674 1 705 1 706 1 701 1 686 2 204 1 889 1 600 1 977 1 955 1 772 1 821 1 820 1632 1553
Co 166 180 176 180 166 164 171 197 176 162 176 173 167 160 166 107 109
Ni 1 834 1 668 1 870 1 906 1 973 2 050 1 870 2 051 2 125 1 783 1 762 1 652 1 638 1 505 1 523 1 418 1 494
Zn 91.2 98.3 103.3 90.6 77.4 80.4 76.0 100.4 79.0 85.6 99.2 145.9 70.9 56.6 74.3 118.3 113.9
Y 0.47 0.35 0.22 0.25 0.60 0.37 0.19 0.95 0.22 0.07 0.12 0.40 0.31 0.19 0.18 0.39 0.19
Zr 0.41 0.04 0.15 0.05 0.35 0.45 0.10 0.17 0.13 0.04 0.02 0.06 0.18 0.26 0.49 0.12 0.08
采样位置 I号岩体上部岩相带
样号 JC06-234 JC06-237 JC13-114 JC13-116 JC13-112 JC13-118 JC13-121
岩性 细粒含硫化物橄榄岩 细粒含硫化物橄榄岩 细粒含硫化物橄榄岩 细粒含硫化物橄榄岩 细粒含硫化物橄榄岩 细粒二辉橄榄岩 细粒橄榄辉石岩
点号 Ol-1 Ol-2 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3
主量元素质量百分含量/% MgO 44.9 45.1 43.7 43.6 43.1 43.1 44.2 43.7 42.2 44.1 43.9 44.0 44.6 43.7 42.8 42.1 43.9 42.0 41.7 42.2
Al2O3 0.0 0.0 0.0 0.1 0.0 0.1 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
SiO2 40.2 39.5 40.6 40.9 40.2 39.9 40.9 40.1 39.3 38.6 40.3 40.2 40.8 40.3 39.4 40.3 40.6 39.1 38.8 39.1
CaO 0.2 0.0 0.0 0.3 0.1 0.3 0.1 0.0 0.1 0.1 0.3 0.0 0.3 0.1 0.1 0.2 0.1 0.1 0.1 0.0
TiO2 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
Cr2O3 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
MnO 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2
FeO 13.4 13.1 14.0 14.1 14.4 15.0 15.0 14.8 14.2 14.4 14.8 14.3 14.9 14.6 15.7 16.5 15.4 17.1 17.1 17.5
Na2O 0.0 0.0 0.0 0.0 0.0 0.0 0.1 0.0 0.0 0.0 0.0 0.0 0.1 0.0 0.0 0.1 0.0 0.0 0.0 0.0
K2O 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
NiO 0.3 0.2 0.3 0.3 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.3 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2
总量 99.2 98.3 98.7 99.6 98.3 98.9 100.8 99.2 96.4 97.8 99.8 99.1 101.2 99.3 98.6 99.6 100.6 98.7 98.2 99.3
Fo 85.6 86.0 84.8 84.7 84.2 83.6 84.0 84.1 84.1 84.5 84.1 84.6 84.2 84.2 83.0 81.9 83.5 81.5 81.3 81.2
微量元素/(μg/g) Li 5.82 3.99 11.93 7.35 6.74 3.41 3.32 3.76 5.93 4.72 5.38 2.62 5.32 3.73 6.16 4.33 6.79 5.32 4.30 7.97
Na 11.5 10.9 25.1 23.3 24.7 86.0 22.1 18.6 690.0 16.3 224.0 23.8 27.9 14.9 8.7 30.2 10.0 12.8 11.3 18.2
Al 120.3 126.5 164.0 91.1 122.6 107.8 109.2 90.9 89.7 136.9 114.5 118.8 151.0 101.3 142.1 173.4 161.9 95.9 111.1 114.8
P 91.8 80.4 204.6 105.6 95.6 57.7 50.1 59.3 64.1 50.5 60.6 66.4 70.9 64.4 72.4 56.9 73.6 67.9 47.0 81.1
Ca 929 741 979 291 889 433 641 603 540 762 1160 867 759 723 858 589 605 900 775 776
Sc 6.26 6.83 6.50 7.05 6.53 2.98 4.97 4.55 3.68 4.53 3.98 5.22 4.61 4.66 3.61 3.82 3.50 3.93 3.71 4.03
Ti 90.4 137 70.5 133 140 137 78.4 118 160 71.1 74.9 90.5 113 152 36.6 44.0 55.0 69.8 91.2 48.8
V 4.44 4.31 4.65 3.23 4.11 6.82 5.55 4.27 4.46 4.91 4.27 4.91 4.59 4.36 3.87 4.09 4.49 4.98 3.88 4.62
Cr 123.8 126.4 127.8 68.3 158.0 66.2 108.9 82.9 80.7 124.1 103.7 97.8 86.7 105.6 105.0 98.4 114.7 88.0 82.6 96.1
Mn 1 596 1 680 1 616 1 823 1 760 1 586 1 657 1 602 1 589 1 621 1 614 1 599 1 736 1 642 1 625 1 931 1 626 1 798 1 810 1 828
Co 166 166 164 99 168 164 173 173 168 168 167 158 176 163 158 170 195 148 157 163
Ni 2 081 2 528 1 961 1 819 2 003 2 026 1 853 1 935 1 747 1 765 1 782 2 152 2 138 2 017 1 921 1 826 1 873 1 559 1 533 1 604
Zn 80.8 67.9 66.3 60.9 70.6 45.4 71.1 82.9 85.9 69.2 82.3 52.0 74.1 97.3 84.9 67.5 57.6 72.8 58.7 57.4
Y 0.27 0.57 0.43 0.22 0.42 0.20 0.27 0.32 0.24 0.22 0.21 0.38 0.48 0.28 0.07 0.07 0.06 0.56 0.43 0.26
Zr 0.04 0.06 0.07 0.50 0.72 0.32 0.16 0.26 0.23 0.11 0.08 0.19 0.24 0.44 0.02 0.05 0.06 0.13 0.19 0.09
采样位置 II号岩体
样号 JC12-201 JC12-207 JC13-259 JC12-206 JC13-258 JC13-259 JC13-254
岩性 中粒橄榄辉石岩 中粒硫化物二辉橄榄岩 中粒二辉橄榄岩 中粒硫化物二辉橄榄岩 中粒二辉橄榄岩 中粒二辉橄榄岩 中粒斜长石二辉橄榄岩
点号 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3 Ol-1 Ol-2 Ol-3

主量元素质量

百分含量/ %

MgO 44.1 42.6 43.4 43.4 43.7 43.6 42.5 42.1 43.2 41.1 42.7 42.3 42.4 41.7 42.7 42.7 42.6 42.1 42.6 41.5 42.4
Al2O3 0.0 0.0 0.0 0.0 0.0 0.1 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
SiO2 39.9 39.3 39.7 39.3 39.4 39.4 40.2 39.2 40.8 38.7 40.1 38.8 39.8 39.6 39.6 39.9 40.7 38.9 38.5 38.5 40.2
CaO 0.0 0.1 0.0 0.0 0.0 0.2 0.2 0.0 0.0 0.0 0.0 0.0 0.0 0.1 0.1 0.0 0.2 0.1 0.1 0.1 0.2
TiO2 0.0 0.1 0.1 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.1 0.0 0.0 0.1 0.0 0.0 0.1 0.1
Cr2O3 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.1 0.0
MnO 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2
FeO 15.1 14.3 15.6 15.4 14.9 14.9 16.1 16.1 15.6 17.0 16.5 16.7 16.9 17.3 16.3 16.2 16.6 16.4 17.1 17.5 16.6
Na2O 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.1 0.0 0.0 0.0 0.0 0.0
K2O 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
NiO 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2 0.2
总量 98.6 96.8 99.3 98.6 98.5 98.6 99.4 97.7 100.1 97.2 99.9 98.3 99.6 99.2 99.1 99.3 100.5 97.9 98.9 98.4 99.8
Fo 83.9 84.1 83.2 83.4 83.9 83.9 82.5 82.4 83.2 81.2 82.2 81.9 81.7 81.2 82.4 82.5 82.1 82.1 81.6 80.8 82.0

微量元素

/(μg/g)

 Li 4.48 6.04 4.76 3.32 6.66 4.78 6.62 5.71 8.22 11.97 3.76 4.98 5.53 4.29 4.38 4.81 6.54 2.13 3.78 4.38 7.92
Na 26.2 8.2 12.4 6.7 5.2 7.3 19.5 44.5 8.7 372.0 17.6 47.6 12.8 9.6 10.1 14.0 12.9 6.5 33.6 77.0 6.3
Al 131.8 75.9 107.5 101.0 53.7 82.3 229.0 62.7 99.2 442.0 86.9 87.8 112.9 91.9 132.1 113.7 98.8 87.3 101.7 123.5 62.7
P 56.8 89.4 62.1 57.9 84.9 52.8 65.4 55.0 68.2 140.1 60.4 59.9 67.1 64.9 70.6 74.8 115.3 45.2 47.8 58.3 108.9
Ca 1035 545 277 305 483 617 676 2440 452 348 629 665 739 697 788 790 577 327 870 316 323
Sc 4.88 4.70 3.65 3.73 3.44 4.37 5.56 4.07 4.71 0.37 4.71 4.81 5.50 4.82 6.25 5.16 4.65 5.40 4.27 5.76 3.34
Ti 76 116 160 133 109 78 132 103 151 55 107 113 118 66 88 53 95 118 137 100 154
V 4.73 2.75 2.63 3.42 1.92 3.27 5.76 2.52 4.04 0.86 5.32 5.67 4.83 4.44 5.40 4.28 3.77 2.66 4.56 4.87 3.27
Cr 106.2 53.2 51.1 68.7 41.0 66.0 164.0 45.1 70.5 42.1 110.9 75.8 73.7 56.5 72.3 55.5 62.1 47.4 60.4 65.1 27.0
Mn 1 704 1 610 1 619 1 554 1 573 1 616 1 691 1 766 1 674 1 642 1 745 1 703 1 733 1 692 1 786 1 738 1 624 1 566 1 812 1 779 1 729
Co 182 167 166 165 168 175 174 169 174 94 115 103 174 171 170 171 171 179 176 163 189
Ni 1 767 1 670 1 635 1 624 1 686 1 679 1 676 1 646 1 715 1 029 1 605 1 605 1 614 1 635 1 571 1 649 1 693 1 778 1 737 1 655 1 882
Zn 100.5 61.3 63.9 65.2 77.3 47.5 73.2 74.3 73.0 72.7 88.5 81.9 97.9 88.7 95.6 74.2 73.2 83.0 74.1 60.5 80.9
Y 0.56 0.36 0.58 0.12 0.17 0.24 0.70 0.29 0.38 0.11 0.31 0.69 0.54 0.36 0.61 0.54 0.29 0.36 0.39 0.23 0.21
Zr 0.21 0.57 0.30 0.40 0.37 0.25 0.62 0.55 0.57 0.25 0.25 0.30 0.39 0.18 0.21 0.09 0.32 0.56 0.54 0.35 0.44
图3 LA-ICP-MS标样分析结果与推荐值比较
Fig.3 Comparison of LA-ICP-MS analytical results with their preferred values
图4 橄榄石中微量元素在岩体和岩相间的变化
Fig.4 Variation of trace elements in olivines with intrusion and petrofacies
图5 金川超镁铁质岩体橄榄石中主要微量元素标准化蛛网图
Fig.5 The original mantle olivine-normalized trace element patterns of the Jinchuan intrusion
图6 金川超镁铁质岩体中橄榄石Fo与微量元素二元相关图
Fig.6 Plots of selected trace elements vs. forsterite content of analyzed olivine
图7 金川超镁铁质岩体橄榄石微量元素地幔源区的判别图（据参考文献 [ 32 , 45 ] 修改）
Fig.7 Discrimination diagrams for the mantle sources of the Jinchuan ultramafic intrusion using the trace elements in olivine (modified after references [ 32 , 45 ])
表2 微量元素 Cr, V, Ni和 Co的分配系数和 Co值
Table 2 Distribution coefficients and Co values of trace elements Cr, V, Ni and Co
Cr V Ni Co
D 硫化物 0.9 0.6 500 70
D 橄榄石 0.9 0.09 7 3.2
D 尖晶石 240 6 2 4.6
Co/(μg/g) 180 50 300 60
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