广西大厂锡多金属矿田西矿带稀散元素铟的富集规律研究—来自矿石组构和闪锌矿地球化学的证据
Enrichment of indium in west ore belt of Dachang orefield: Evidence from ore textures and sphalerite geochemistry
查看参考文献34篇
文摘
|
广西大厂锡多金属矿田是世界最主要的铟产地之一,对其的富集机制还有很大争议。文章以大厂矿田西矿带高峰矿床和铜坑矿床中的闪锌矿为研究对象,在野外和室内矿相显微观察的基础上,应用高精度电子探针与等离子体质谱分析手段,研究稀散元素铟的空间分布规律、赋存状态及与主成矿元素的关系,揭示其在闪锌矿中的富集规律。实验结果表明,铜坑矿床中闪锌矿内稀散元素铟的含量随深度增加而减少,而高峰矿床中铟含量却保持稳定;铟主要以类质同象形式赋存,与铜以双替代锌的形式进入闪锌矿晶格中,也不排除铟以微细包体形式赋存的可能。结合前人研究,推断燕山晚期复式岩体岩浆演化末期花岗斑岩侵位冷却过程中,岩浆结晶产生的富铟、铜等流体对早期生成的闪锌矿进行交代并富集。这一研究结果为寻找稀散元素铟指示了方向。 |
其他语种文摘
|
The Dachang tin-polymetallic deposit in northwestern Guangxi contains large amounts of indium. The mechanisms of indium concentration are rather complex and remain unclear. In this study, the spatial distribution of various elements (including indium), their modes of occurrence, and their relationship with the main oreforming elements were investigated. Based on field investigation and microscopic observation, the authors conducted ion-coupled plasma mass spectroscopy and electron microprobe analysis of indium in sphalerite from the tin-polymetallic sulfide deposits of the Dachang orefield. The results show that the concentration of scattered element indium in sphalerite of the Tongkeng deposit decreases with the depth, whereas it is stable in the Gaofeng deposit. Indium isomorphically occurs in sphalerite, and there is a positive correlation between In and Cu, supporting the argument for coupled substitution : In~(3+) +Cu~+ →2Zn~(2+), although it may also be present in sub-microinclusions. Combined with previous studies, it is concluded that In, Cu, and Sn-bearing fluids were exsolved from the cooling granite porphyry magma and formed In-bearing sphalerite by replacement of the pre-existing sphalerite. These results provide guidance for future indium exploration. |
来源
|
矿床地质
,2015,34(2):379-396 【核心库】
|
DOI
|
10.16111/j.0258-7106.2015.02.012
|
关键词
|
地球化学
;
稀散元素铟
;
类质同象
;
双替代
;
大厂锡多金属矿田
|
地址
|
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, 550002
2.
中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室, 北京, 100037
3.
桂林理工大学广西矿冶与环境科学实验中心, 广西, 桂林, 541004
|
语种
|
中文 |
文献类型
|
研究性论文 |
ISSN
|
0258-7106 |
学科
|
地质学 |
基金
|
中国三稀金属资源战略调查
;
博士启动基金
|
文献收藏号
|
CSCD:5397975
|
参考文献 共
34
共2页
|
1.
Barton P B Jr. Some ore textures involving sphalerite from the Furutobe mine, akita prefecture, Japan.
Mining Geology,1987,28:293-300
|
CSCD被引
1
次
|
|
|
|
2.
Benzaazoua M. Tin and indium mineralogy within selected sampes from the Neves Corvo ore deosit(Portugal): A multidisciplinary study.
Mineral Eng,2003,16(11,suppl1):1291-1302
|
CSCD被引
10
次
|
|
|
|
3.
蔡明海. 广西大厂锡矿田侵入岩SHRIMP锆石U-Pb年龄及其意义.
地质论评,2006,52(3):409-414
|
CSCD被引
70
次
|
|
|
|
4.
成永生. 广西大厂矿田大福楼锡多金属矿床地质与地球化学特征.
中国有色金属学报,2012,22(3):751-760
|
CSCD被引
6
次
|
|
|
|
5.
Cook N J. Trace and minor elements in sphalerite: A LA-ICPMS study.
Geochimica et Cosmochimica Acta,2009,73:4761-479
|
CSCD被引
143
次
|
|
|
|
6.
范森葵. 广西大厂矿田矿床分布规律与找矿方向.
矿产与地质,2008,22(6):520-524
|
CSCD被引
3
次
|
|
|
|
7.
范森葵. 广西大厂矿区脉岩的地球化学特征及其构造和成矿意义.
地质与勘探,2010,46(5):828-835
|
CSCD被引
8
次
|
|
|
|
8.
韩发. 大厂锡-多金属矿床喷气沉积成因的证据--矿床地质、地球化学特征.
矿床地质,1990,9(4):309-324
|
CSCD被引
18
次
|
|
|
|
9.
Harald G D. Sulfidic and non-sulfidic indium mineralization of the epithermal Au-Cu-Zn-Pb-Ag deposit San Roque (Provincia Rio Negro, SE Argentina)-with special reference to the " indium window" in zinc sulfide.
Ore Geology Reviews,2013,52:103-128
|
CSCD被引
2
次
|
|
|
|
10.
Hiroyasu M. Trace elements of Indium-bearing sphalerite from tin-polymetallic deposits in Bolivia,China and Japan: A femto-second LA-ICPMS study.
Ore Geology Reviews,2013,53:103-128
|
CSCD被引
29
次
|
|
|
|
11.
Ishihara S. Indium and other trace elements in volcanogenic massive sulphide ores from the Kuroko, Besshi and other types in Japan.
Bulletin,Geological Survey of Japan,2007,58:7-22
|
CSCD被引
3
次
|
|
|
|
12.
Ishihara S. Indium concentration in zinc ores in plutonic and volcanic environments: Examples at the Dulong and Dachang mines, south China.
Bulletin Geological Survey of Japan,2011,62:259-272
|
CSCD被引
2
次
|
|
|
|
13.
Ishihara S. Inferred indium resources of the Bolivian tin-polymetallic deposits.
Resource Geology,2011,61:174-191
|
CSCD被引
9
次
|
|
|
|
14.
李晓峰. 铟矿床研究现状及其展望.
矿床地质,2007,26(4):475-480
|
CSCD被引
27
次
|
|
|
|
15.
李晓峰. 广西大厂锡矿铟的地球化学特征及成因机制初探.
矿床地质,2010,29(5):903-914
|
CSCD被引
23
次
|
|
|
|
16.
梁婷. 广西大厂锡多金属矿床S、Pb同位素组成对成矿物质来源的示踪.
地质学报,2008,82(7):967-977
|
CSCD被引
25
次
|
|
|
|
17.
梁婷. 广西大厂笼箱盖复式岩体的LA-MC-ICP-MS锆石U-Pb年龄及其地质意义.
岩石学报,2011,27(1):1624-1636
|
CSCD被引
33
次
|
|
|
|
18.
刘铁庚. 闪锌矿中的Cd主要置换Fe是而不是Zn.
矿物学报,2010,30(2):283-284
|
CSCD被引
2
次
|
|
|
|
19.
Schwarz-Schampera U.
Indium geology,mineralogy, and economics,2002:257
|
CSCD被引
1
次
|
|
|
|
20.
Shimizu T. Hydrothermal alteration and K-Ar ages of Neogene-Quaternary magmatic-hydrothermal systems at Toyoha-Muine area in southwest Hokkaido, Japan.
Resourse Geology,2011,61:192-209
|
CSCD被引
2
次
|
|
|
|
|