100 MPa/800 ℃下Mo和W在流体/花岗质熔体相间分配的实验研究
An experimental study on the partitioning of molybdenum and tungsten between granitic melt and coexisting aqueous fluid at 100 MPa and 800 ℃
查看参考文献41篇
文摘
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利用“RQV-快速内冷淬火”(外加热冷封式)高温高压实验装置,在100 MPa、800 ℃条件下,以东秦岭地区出露的高钾钙碱性岩浆岩(合峪花岗岩)为实验初始物,实验研究了Mo和W在花岗岩-H_2O、花岗岩-NaCl(KCl)-H_2O及花岗岩-NaF-H_2O体系流体/熔体相间的分配行为。实验结果表明,Mo比W更倾向于分配进入流体相(D~(流体/熔体)_(Mo)>>D~(流体/熔体)_W),相对于纯水体系而言,流体介质中Cl和F的存在均有利于Mo和W向流体相迁移富集;随体系内C1含量的不断增高,Mo和W的分配系数呈线性增大趋势;而在天然花岗岩可能含有的F含量范围之内,F含量的增高将阻碍Mo、W向流体相迁移;流体介质中Na/K(摩尔比)的变化对Mo和W的分配系数没有明显影响,表明体系碱质(Na或K)类型不是Mo和W在流体/熔体相间分配的主要影响因素。 |
其他语种文摘
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An experimental study has been conducted to investigate the effect of fluid composition on the partitioning behavior of Mo and W between granitic melts and coexisting aqueous fluid at 100 MPa and 800 ℃. High-K, calc-alkaline granites of the East Qinling molybdenum belt were used as starting materials, and the system of granite-H_2O, granite-NaCl(KCl)-H_2O and granite-NaF-H_2O were investigated. All runs were conducted in cold-seal Rapid-Quench pressure Vessels (RQV, a kind of "externally heated cold-seal pressure vessels") using water as a pressure medium. The results showed that molybdenum was more likely to distribute into the aqueous phase than tungsten (D~(fluid/melt)_Mo>>D~(fluid/melt)_W). In contrast to pure water, the existence of Cl and F in the aqueous promotes the distribution of Mo and W into the fluid phase; The partition coefficients of Mo and W increases linearly with increasing Cl concentration, while the increase of F concentration, within the scope of natural granites, hinders Mo and W to move to the fluid phase. The variation of Na/K value (mole ratio) in the aqueous phase had little effect on the partition coefficients of Mo and W, which indicates that the alkaline type of the system was not the main factor that influences the partitioning behavior of Mo and W between granitic melt and coexisting aqueous fluid. |
来源
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地球化学
,2011,40(6):516-524 【核心库】
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关键词
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分配系数
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流体/熔体作用
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Mo-W
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高温高压实验
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地址
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1.
中国科学院地球化学研究所地球深部物质与流体作用地球化学研究室, 贵州, 贵阳, 550002
2.
有色金属华东地质勘查局, 江苏, 南京, 210007
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语种
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中文 |
文献类型
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研究性论文 |
ISSN
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0379-1726 |
学科
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地质学 |
基金
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国家973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:4415518
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参考文献 共
41
共3页
|
1.
Ryabchikov I D. Mobilization of molybdenum by fluids during the crystallization of granite melts.
Geochem Int,1981,18(4):183-186
|
CSCD被引
3
次
|
|
|
|
2.
Khitarov N I. The distribution of Zn, Cu, Pb and Mo between a fluid phase and a silicate melt of granitic composition at high temperature and pressures.
Geochem Int,1982,19(4):123-136
|
CSCD被引
8
次
|
|
|
|
3.
Candela P A. The partitioning of copper and molybdenum between silicate melts and aqueous fluids.
Geochim Cosmochim Acta,1984,48(2):373-380
|
CSCD被引
74
次
|
|
|
|
4.
Manning D A C. The behaviour of tungsten in granitic melt-vapour systems.
Contrib Mineral Petrol,1984,86(3):286-293
|
CSCD被引
24
次
|
|
|
|
5.
Keppler H. Partitioning of Cu, Sn, Mo, W, U, and Th between melt and aqueous fluid in the systems haplogranite-H20-HCl and haplogranite-H20-HF.
Contrib Mineral Petrol,1991,109(2):139150
|
CSCD被引
1
次
|
|
|
|
6.
许永胜. 钨在水流体和硅酸盐熔体相间分配的实验研究.
地球化学,1992,21(3):273-281
|
CSCD被引
4
次
|
|
|
|
7.
赵斌.
高温高压实验地球化学,1995:1-267
|
CSCD被引
8
次
|
|
|
|
8.
Bai T B. The distribution of Na, K, Rb, Sr, AI, Ge, Cu, W, Mo, La, and Ce between granitic melts and coexisting aqueous fluids.
Geochim Cosmochim Acta,1999,63(7/8):1117-1131
|
CSCD被引
40
次
|
|
|
|
9.
唐群力. 硅酸盐熔/流共存体系中元素分配系数研究的几个问题.
地质地球化学,2003,31(3):88-92
|
CSCD被引
2
次
|
|
|
|
10.
黄典豪. 东秦岭地区钼矿床的铼-锇同位素年龄及其意义.
矿床地质,1994,13(3):221-230
|
CSCD被引
170
次
|
|
|
|
11.
Fan Hongrui. Porphyry-type molybdenum deposits in the eastern Qinling Mo belt, central China.
Sci Geol Sinica,1999,8(1):91-101
|
CSCD被引
4
次
|
|
|
|
12.
李永峰. 东秦岭钼矿类型、特征、成矿时代及其地球动力学背景.
矿床地质,2005,22(3):292-304
|
CSCD被引
142
次
|
|
|
|
13.
付治国. 东沟钼矿矿床地质特征及找矿因素研究.
中国钼业,2005,29(2):8-16
|
CSCD被引
18
次
|
|
|
|
14.
叶会寿. 东秦岭东沟超大型斑岩钼矿SHRIMP锆石U—Pb和辉钼矿Re—Os年龄及其地质意义.
地质学报,2006,80(7):1078-1088
|
CSCD被引
136
次
|
|
|
|
15.
李诺. 东秦岭斑岩钼矿带的地质特征和成矿构造背景.
地学前缘,2007,14(5):186-198
|
CSCD被引
144
次
|
|
|
|
16.
陈衍景. 不同类型热液金矿系统的流体包裹体特征.
岩石学报,2007,23(9):2085-2108
|
CSCD被引
423
次
|
|
|
|
17.
邓小华. 河南嵩县纸房钼矿床流体包裹体研究及矿床成因.
岩石学报,2008,24(9):2133-2148
|
CSCD被引
40
次
|
|
|
|
18.
倪智勇. 河南小秦岭金矿田大湖金-钼矿床流体包裹体特征及矿床成因.
岩石学报,2008,24(9):2058-2068
|
CSCD被引
29
次
|
|
|
|
19.
王运. 河南省商城县汤家坪钼矿床地质和流体包裹体研究.
岩石学报,2009,25(2):468-480
|
CSCD被引
36
次
|
|
|
|
20.
Chou I M. Oxygen buffer and hydrogen sensor techniques at elevated pressure and temperature.
Hydrothermal Experimental Techniques,1987:61-69
|
CSCD被引
11
次
|
|
|
|
|