稀有金属矿物溶解度对花岗伟晶岩成矿作用的制约

doi:10.13745/j.esf.sf.2021.8.7

地学前缘 ›› 2022, Vol. 29 ›› Issue (1): 81-92.DOI: 10.13745/j.esf.sf.2021.8.7

• 稀有金属矿床成矿过程及勘查进展 • 上一篇下一篇

稀有金属矿物溶解度对花岗伟晶岩成矿作用的制约

唐勇¹(), 覃山县¹^,², 赵景宇³, 吕正航¹, 刘喜强¹^,², 王宏¹^,², 陈剑争¹^,², 张辉¹^,^*()

1.中国科学院地球化学研究所地球内部物质高温高压院重点实验室, 贵州贵阳 550081
2.中国科学院大学, 北京 100049
3.宿州学院资源与土木工程学院, 安徽宿州 234000

收稿日期:2020-06-20 修回日期:2021-01-22 出版日期:2022-01-25 发布日期:2022-02-22
通讯作者: 张辉
作者简介:唐勇(1980—),男,研究员,博士生导师,主要从事伟晶岩成矿与找矿研究。E-mail: tangyong@vip.gyig.ac.cn
基金资助:
国家自然科学基金项目(41773053);国家自然科学基金项目(91962222)

Solubility of rare metals as a constraint on mineralization of granitic pegmatite

TANG Yong¹(), QIN Shanxian¹^,², ZHAO Jingyu³, LÜ Zhenghang¹, LIU Xiqiang¹^,², WANG Hong¹^,², CHEN Jianzheng¹^,², ZHANG Hui¹^,^*()

1. Key Laboratory of High-Temperature and High-Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
2. University of the Chinese Academy of Sciences, Beijing 100049, China
3. School of Resources and Civil Engineering, Suzhou University, Suzhou 234000, China

Received:2020-06-20 Revised:2021-01-22 Online:2022-01-25 Published:2022-02-22
Contact: ZHANG Hui

摘要/Abstract

摘要：

花岗伟晶岩型矿床是稀有金属矿床重要的类型之一。在花岗伟晶岩中,稀有金属元素Li、Be、Nb和Ta主要以独立矿物的形式存在,前人对稀有金属独立矿物在硅酸盐熔体中的溶解度及其影响因素展开了系统研究。本文综合分析了已有的实验数据,其结果表明,影响稀有金属独立矿物溶解度最为重要的2个参数是温度(T)和铝饱和指数(ASI)。因此本文建立了稀有金属独立矿物,尤其是铌锰矿和钽锰矿溶解度,与温度(T)和铝饱和指数(ASI)之间的定量关系:
lg [w(Li)/10^-6]=-0.37×[1 000/(T/K)]+4.56,R²=0.44
lg [w(BeO)/10^-6]=-4.21×[1 000/(T/K)]+6.86,R²=0.91
lg [K_sp(Nb)/(mg²·kg^-2)]=-(2.86±0.14)×ASI_(Mn+Li)-(4.95±0.31)×[1 000/(T/K)]+(4.20+0.28),R²=0.86
lg [K_sp(Ta)/(mg²·kg^-2)]=-(2.46±0.11)×ASI_(Mn+Li)-(4.86±0.30)×[1 000/(T/K)]+(4.00+0.30),R²=0.80
式中,温度T为热力学温度,ASI_(Mn+Li)(ASI=Al₂O₃/(CaO+Na₂O+K₂O+Li₂O+MnO),摩尔分数比)和T的适用范围分别为0.6~1.2和1 073~1 373 K的范围内。上述公式为估算硅酸盐熔体中稀有金属含量提供了便利,为量化花岗伟晶岩成矿模型提供了基础。
稀有金属独立矿物溶解度随温度降低和铝饱和指数的增加而急剧降低,因此,在岩浆演化过程中,由岩浆侵位、分离结晶以及流体作用等因素引起的岩浆温度降低和铝饱和指数的增加,是导致稀有金属独立矿物结晶的主要机制。

关键词: 稀有金属矿物, 溶解度, 温度, 铝饱和指数, 伟晶岩

Abstract:

Granitic pegmatite deposit is one of important types of rare metal deposits. In the granitic pegmatite, the rare metals Li, Be, Nb and Ta mainly occur in mineralogically distinct zones. Their solubilities in silicate melts have been studied systematically and shown to be mostly affected by temperature (T) and aluminum saturation index (ASI). Here we set out to establish quantitative relationships between T/ASI and the solubility of rare metal minerals (Nb and Ta) in silicate melts by multiple linear regression analysis of literature data. We found the following relationships:
lgc(Li) (10^-6)=-0.37×(1000/T)+4.56, R²=0.44
lgc(BeO) (10^-6)=-4.21×(1000/T)+6.86, R²=0.91
lgK_sp(Nb)=-(2.86±0.14)×ASI_(Mn+Li)(4.95±0.31)×(1000/T)+(4.20+0.28), R²=0.86
lgK_sp(Ta)=-(2.46±0.11)×ASI_(Mn+Li)(4.86±0.30)×(1000/T)+(4.00+0.30), R²=0.80
Where c is percentage content; K_sp is solubility, in mg ²/kg²; ASI_(Mn+Li) is the molar ratio Al₂O₃/(CaO+Na₂O+K₂O+Li₂O+MnO), applicable between 0.6-1.2; and T is temperature of silicate melt in Kelvin, applicable between 1073-1373 K. These quantitative relationships can be used as a basis for quantifying the metallogenic model of granitic pegmatite. The sharply decrease of solubility with decreasing T and increasing ASI can be the main mechanism leading to the crystallization of rare metal minerals, because the same conditions are met during magma evolution, where magma emplacement, fractional crystallization and fluid-melt interaction cause increase of magma temperature and decrease of ASI.

Key words: rare metal minerals, solubility, temperature, ASI, pegmatite

中图分类号:

唐勇, 覃山县, 赵景宇, 吕正航, 刘喜强, 王宏, 陈剑争, 张辉. 稀有金属矿物溶解度对花岗伟晶岩成矿作用的制约[J]. 地学前缘, 2022, 29(1): 81-92.

TANG Yong, QIN Shanxian, ZHAO Jingyu, LÜ Zhenghang, LIU Xiqiang, WANG Hong, CHEN Jianzheng, ZHANG Hui. Solubility of rare metals as a constraint on mineralization of granitic pegmatite[J]. Earth Science Frontiers, 2022, 29(1): 81-92.

图/表 6

图1 挥发组分对铌锰矿和钽锰矿溶解度的影响 (数据引自文献[10,12,14-15])

Fig.1 Effect of flux elements on the solubility of Mn-columbite and Mn-tantalite. Data adapted from [10,12,14-15].

图2 温度对稀有金属独立矿物溶解度的影响 (数据引自文献[10-13,15-21])

Fig.2 Effect of temperature on the solubility of independent rare-metal minerals. Data adapted from [10-13,15-21].

表1 温度对稀有金属矿物溶解度影响 (数据引自[10-13,15-21])

Table 1 Effect of temperature on solubility of rare metal minerals. Data adapted from [10-13,15-21].

序号	ASI	矿物	等式	R²	斜率	H/(kJ·mol^-1)
1	1.00	锂辉石	lg [w(Li)/10^-6]=-0.37×[1 000/(T/K)]+4.56	0.44	0.37	7.1
2	1.00	绿柱石	lg [w(BeO)/10^-6] =-2.75×[1 000/(T/K)]+5.89	0.95	3.32	63.6
3	>1.00	绿柱石	lg [w(BeO)/10^-6] =-4.21×[1 000/(T/K)]+6.86	0.91	4.21	80.6
4	0.60	铌锰矿	lg [ $K sp Nb$ /(mol²·kg^-2)]=-2.32×[1 000/(T/K)]+0.42	0.78	2.32	44.4
5	1.00	铌锰矿	lg [ $K sp Nb$ /(mol²·kg^-2)]=-5.56×[1 000/(T/K)]+1.75	0.98	5.56	106.5
6	1.20	铌锰矿	lg [ $K sp Nb$ /(mol²·kg^-2)]=-8.06×[1 000/(T/K)]+3.73	1.00	8.06	154.3
7	0.90	钽锰矿	lg [ $K sp Ta$ /(mol²·kg^-2)]=-5.28×[1 000/(T/K)]+2.24	0.98	5.28	101.1
8	1.00	钽锰矿	lg [ $K sp Ta$ /(mol²·kg^-2)]=-7.01×[1 000/(T/K)]+3.17	0.94	7.01	134.2
9	1.10	钽锰矿	lg [ $K sp Ta$ /(mol²·kg^-2)]=-5.19×[1 000/(T/K)]+3.17	0.94	5.19	99.4

表1 温度对稀有金属矿物溶解度影响 (数据引自[10-13,15-21])

Table 1 Effect of temperature on solubility of rare metal minerals. Data adapted from [10-13,15-21].

序号	ASI	矿物	等式	R²	斜率	H/(kJ·mol^-1)
1	1.00	锂辉石	lg [w(Li)/10^-6]=-0.37×[1 000/(T/K)]+4.56	0.44	0.37	7.1
2	1.00	绿柱石	lg [w(BeO)/10^-6] =-2.75×[1 000/(T/K)]+5.89	0.95	3.32	63.6
3	>1.00	绿柱石	lg [w(BeO)/10^-6] =-4.21×[1 000/(T/K)]+6.86	0.91	4.21	80.6
4	0.60	铌锰矿	lg [ $K sp Nb$ /(mol²·kg^-2)]=-2.32×[1 000/(T/K)]+0.42	0.78	2.32	44.4
5	1.00	铌锰矿	lg [ $K sp Nb$ /(mol²·kg^-2)]=-5.56×[1 000/(T/K)]+1.75	0.98	5.56	106.5
6	1.20	铌锰矿	lg [ $K sp Nb$ /(mol²·kg^-2)]=-8.06×[1 000/(T/K)]+3.73	1.00	8.06	154.3
7	0.90	钽锰矿	lg [ $K sp Ta$ /(mol²·kg^-2)]=-5.28×[1 000/(T/K)]+2.24	0.98	5.28	101.1
8	1.00	钽锰矿	lg [ $K sp Ta$ /(mol²·kg^-2)]=-7.01×[1 000/(T/K)]+3.17	0.94	7.01	134.2
9	1.10	钽锰矿	lg [ $K sp Ta$ /(mol²·kg^-2)]=-5.19×[1 000/(T/K)]+3.17	0.94	5.19	99.4

图3 熔体组成(ASI)对绿柱石、铌锰矿和钽锰矿溶解度的影响 (数据引自文献[10-13,15-20,22])

Fig.3 Effect of melt composition (ASI) on the solubility of beryl, Mn-columbite and Mn-tantalite. Data adapted from [10-13,15-20,22].

图4 稀有金属矿物饱和结晶及其在伟晶岩中分布特征 (据文献[30]修改)

Fig.4 Distribution of rare metals in granitic pegmatite. Modified after [30].

图5 稀有金属元素溶解度-温度的关系图 a—甲基卡X03伟晶岩脉中Li2O含量最大为1.5%;b—伟晶岩中已知最低和平均Be含量分别为30×10-6和200×10-6;c,d—熔体MnO含量受锰铝榴石的控制,熔体中MnO含量与温度的关系[31]为:ln[MnO]=-9 747.4/(T/K)+5.24,T为热力学温度。Tanco伟晶岩全岩铌和钽的含量分别为56×10-6和300×10-6。

Fig.5 Temperature-solubility diagrams for Li, Be, Nb and Ta

参考文献 71

[1]	LINNEN R L, SAMSON I M, WILLIAMS-JONES A E, et al. Geochemistry of the rare-earth element, Nb, Ta, Hf, and Zr deposits[M]// Treatise on geochemistry. Amsterdam: Elsevier, 2014: 543-568.
[2]	LINNEN R L, VAN LICHTERVELDE M, ČERNÝ P. Granitic pegmatites as sources of strategic metals[J]. Elements, 2012, 8(4):275-280. DOI URL
[3]	LIN Y, POLLARD P J, HU S X, et al. Geologic and geochemical characteristics of the Yichun Ta-Nb-Li deposit, Jiangxi Province, South China[J]. Economic Geology, 1995, 90(3):577-585. DOI URL
[4]	王汝成, 吴福元, 谢磊, 等. 藏南喜马拉雅淡色花岗岩稀有金属成矿作用初步研究[J]. 中国科学:地球科学, 2017, 47(8):871-880.
[5]	吴福元, 刘志超, 刘小驰, 等. 喜马拉雅淡色花岗岩[J]. 岩石学报, 2015, 31(1):1-36.
[6]	张辉, 吕正航, 唐勇. 新疆阿尔泰造山带中伟晶岩型稀有金属矿床成矿规律、找矿模型及其找矿方向[J]. 矿床地质, 2019, 38(4):792-814.
[7]	XU Z Q, FU X F, WANG R C, et al. Generation of lithium-bearing pegmatite deposits within the Songpan-Ganze orogenic belt, East Tibet[J]. Lithos, 2020, 354/355:105281. DOI URL
[8]	WANG H, GAO H, ZHANG X Y, et al. Geology and geochronology of the super-large Bailongshan Li-Rb-(Be) rare-metal pegmatite deposit, West Kunlun orogenic belt, NW China[J]. Lithos, 2020, 360/361:105449. DOI URL
[9]	XIONG Y Q, JIANG S Y, WEN C H, et al. Granite-pegmatite connection and mineralization age of the giant Renli Ta-Nb deposit in South China: constraints from U-Th-Pb geochronology of coltan, monazite, and zircon[J]. Lithos, 2020, 358/359:105422. DOI URL
[10]	ASERI A A, LINNEN R L, CHE X D, et al. Effects of fluorine on the solubilities of Nb, Ta, Zr and Hf minerals in highly fluxed water-saturated haplogranitic melts[J]. Ore Geology Reviews, 2015, 64:736-746. DOI URL
[11]	BARTELS A, HOLTZ F, LINNEN R L. Solubility of manganotantalite and manganocolumbite in pegmatitic melts[J]. American Mineralogist, 2010, 95(4):537-544. DOI URL
[12]	FIEGE A, KIRCHNER C, HOLTZ F, et al. Influence of fluorine on the solubility of manganotantalite (MnTa₂O₆) and manganocolumbite (MnNb₂O₆) in granitic melts: an experimental study[J]. Lithos, 2011, 122(3/4):165-174. DOI URL
[13]	FIEGE A, SIMON A, LINSLER S A, et al. Experimental constraints on the effect of phosphorous and boron on Nb and Ta ore formation[J]. Ore Geology Reviews, 2018, 94:383-395. DOI URL
[14]	KEPPLER H. Influence of fluorine on the enrichment of high field strength trace elements in granitic rocks[J]. Contributions to Mineralogy and Petrology, 1993, 114(4):479-488. DOI URL
[15]	LINNEN R L. The solubility of Nb-Ta-Zr-Hf-W in granitic melts with Li and Li + F: constraints for mineralization in rare metal granites and pegmatites[J]. Economic Geology, 1998, 93(7):1013-1025. DOI URL
[16]	LINNEN R L. The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts[J]. Lithos, 2005, 80(1/2/3/4):267-280. DOI URL
[17]	LINNEN R L, KEPPLER H. Columbite solubility in granitic melts: consequences for the enrichment and fractionation of Nb and Ta in the Earth’s crust[J]. Contributions to Mineralogy and Petrology, 1997, 128(2/3):213-227. DOI URL
[18]	TANG Y, ZHANG H, RAO B. The effect of phosphorus on manganocolumbite and mangaotantalite solubility in peralkaline to peraluminous granitic melts[J]. American Mineralogist, 2016, 101(2):415-422. DOI URL
[19]	CHEVYCHELOV V Y, BORODULIN G P, ZARAISKY G P. Solubility of columbite, (Mn, Fe)(Nb, Ta)₂O₆, in granitoid and alkaline melts at 650-850 ℃ and 30-400 MPa: an experimental investigation[J]. Geochemistry International, 2010, 48(5):456-464. DOI URL
[20]	EVENSEN J M, LONDON D, WENDLANDT R F. Solubility and stability of beryl in granitic melts[J]. American Mineralogist, 1999, 84(5/6):733-745. DOI URL
[21]	MANETA V, BAKER D R, MINARIK W. Evidence for lithium-aluminosilicate supersaturation of pegmatite-forming melts[J]. Contributions to Mineralogy and Petrology, 2015, 170(1):1-16. DOI URL
[22]	VAN LICHTERVELDE M, HOLTZ F, HANCHAR J M. Solubility of manganotantalite, zircon and hafnon in highly fluxed peralkaline to peraluminous pegmatitic melts[J]. Contributions to Mineralogy and Petrology, 2010, 160(1):17-32. DOI URL
[23]	STEWART D B. Petrogenesis of lithium-rich pegmatites[J]. American Mineralogist, 1978, 63:970-980.
[24]	LONDON D, MORGAN G B. Experimental crystallization of the Macusani obsidian, with applications to lithium-rich granitic pegmatites[J]. Journal of Petrology, 2017, 58(5):1005-1030. DOI URL
[25]	LONDON D. Experimental phase equilibria in the system LiAlSiO₄-SiO₂-H₂O: a petrogenetic grid for lithium-rich pegmatites[J]. American Mineralogist, 1984, 69(11/12):995-1004.
[26]	张辉. 岩浆-热液过渡阶段体系中不相容元素地球化学行为及其机制: 以新疆阿尔泰3号伟晶岩脉研究为例[D]. 贵阳: 中国科学院地球化学研究所, 2001.
[27]	邹天人, 李庆昌. 中国新疆稀有及稀土金属矿床[M]. 北京: 地质出版社, 2006.
[28]	饶灿. 福建南平31号花岗伟晶岩的矿物学研究与岩浆-热液演化示踪[D]. 南京: 南京大学, 2009.
[29]	ČERNÝ P, ERCIT T S. The classification of granitic pegmatites revisited[J]. The Canadian Mineralogist, 2005, 43(6):2005-2026. DOI URL
[30]	EVENSEN J M, LONDON D. Experimental silicate mineral/melt partition coefficients for beryllium and the crustal Be cycle from migmatite to pegmatite[J]. Geochimica et Cosmochimica Acta, 2002, 66(12):2239-2265. DOI URL
[31]	MANER J L IV, LONDON D, ICENHOWER J P. Enrichment of manganese to spessartine saturation in granite-pegmatite systems[J]. American Mineralogist, 2019, 104(11):1625-1637. DOI URL
[32]	TENG F Z, MCDONOUGH W F, RUDNICK R L, et al. Lithium isotopic composition and concentration of the upper continental crust[J]. Geochimica et Cosmochimica Acta, 2004, 68(20):4167-4178. DOI URL
[33]	TOMASCAK P B, MAGNA T, DOHMEN R. Lithium in the deep earth: mantle and crustal systems[M]// Advances in lithium isotope geochemistry. Berlin: Springer, 2016: 119-156.
[34]	付小芳, 侯立玮, 梁斌, 等. 甲基卡式花岗伟晶岩型锂矿床成矿模式与三维勘查找矿模型[M]. 北京: 科学出版社, 2017.
[35]	LONDON D, MORGAN G B, HERVIG R L. Vapor-undersaturated experiments with Macusani glass+H₂O at 200 MPa, and the internal differentiation of granitic pegmatites[J]. Contributions to Mineralogy and Petrology, 1989, 102(1):1-17. DOI URL
[36]	STILLING A, ČERNÝ P, VANSTONE P J. The Tanco pegmatite at Bernic Lake, Manitoba. XVI. Zonal and bulk compositions and their petrogenetic significance[J]. The Canadian Mineralogist, 2006, 44(3):599-623. DOI URL
[37]	TAYLOR S R, MCLENNAN S M. The geochemical evolution of the continental crust[J]. Reviews of Geophysics, 1995, 33(2):241-265. DOI URL
[38]	GREW E S. Beryllium in metamorphic environments (emphasis on aluminous compositions)[J]. Reviews in Mineralogy and Geochemistry, 2002, 50(1):487-549. DOI URL
[39]	LONDON D, EVENSEN J M. Beryllium in silicic magmas and the origin of beryl-bearing pegmatites[J]. Reviews in Mineralogy and Geochemistry, 2002, 50(1):445-486. DOI URL
[40]	WEBSTER J D, THOMAS R, RHEDE D, et al. Melt inclusions in quartz from an evolved peraluminous pegmatite: geochemical evidence for strong tin enrichment in fluorine-rich and phosphorus-rich residual liquids[J]. Geochimica et Cosmochimica Acta, 1997, 61(13):2589-2604. DOI URL
[41]	CUNEY M, MARIGNAC C, WEISBROD A. The Beauvoir topaz-lepidolite albite granite (Massif Central, France): the disseminated magmatic Sn-Li-Ta-Nb-Be mineralization[J]. Economic Geology, 1992, 87(7):1766-1794. DOI URL
[42]	MCNEIL A G. Crystallization processes and solubility of columbite-(Mn), tantalite-(Mn), microlite, pyrochlore, wodginite and titanowodginite in highly fluxed haplogranitic melts[D]. London: The university of Western Ontario, 2018.
[43]	ZAJACZ Z, HALTER W E, PETTKE T, et al. Determination of fluid/melt partition coefficients by LA-ICPMS analysis of co-existing fluid and silicate melt inclusions: controls on element partitioning[J]. Geochimica et Cosmochimica Acta, 2008, 72(8):2169-2197. DOI URL
[44]	COLOMBO F, SFRAGULLA J, DEL TÁNAGO J G. The garnet-phosphate buffer in peraluminous granitic magmas: a case study from pegmatites in the Pocho District, Córdoba, Argentina[J]. The Canadian Mineralogist, 2012, 50(6):1555-1571. DOI URL
[45]	GAMMEL E M, NABELEK P I. Fluid inclusion examination of the transition from magmatic to hydrothermal conditions in pegmatites from San Diego County, California[J]. American Mineralogist, 2016, 101(8):1906-1915. DOI URL
[46]	KONTAK D J, DOSTAL J, KYSER T K, et al. A petrological, geochemical, isotopic and fluid-inclusion study of 370 Ma pegmatite-aplite sheets, Peggys Cove, Nova Scotia, Canada[J]. The Canadian Mineralogist, 2002, 40(5):1249-1286. DOI URL
[47]	LONDON D, HUNT L E, SCHWING C R, et al. Feldspar thermometry in pegmatites: truth and consequences[J]. Contributions to Mineralogy and Petrology, 2019, 175(1):1-21. DOI URL
[48]	MORGAN VI G B, LONDON D. Crystallization of the Little Three layered pegmatite-aplite dike, Ramona District, California[J]. Contributions to Mineralogy and Petrology, 1999, 136(4):310-330. DOI URL
[49]	SIEGEL K, WAGNER T, TRUMBULL R B, et al. Stable isotope (B, H, O) and mineral-chemistry constraints on the magmatic to hydrothermal evolution of the Varuträsk rare-element pegmatite (Northern Sweden)[J]. Chemical Geology, 2016, 421:1-16. DOI URL
[50]	CHAPPELL B W. Aluminium saturation in I- and S-type granites and the characterization of fractionated haplogranites[J]. Lithos, 1999, 46(3):535-551. DOI URL
[51]	ACOSTA-VIGIL A, LONDON D, MORGAN G B, et al. Solubility of excess alumina in hydrous granitic melts in equilibrium with peraluminous minerals at 700-800 ℃ and 200 MPa, and applications of the aluminum saturation index[J]. Contributions to Mineralogy and Petrology, 2003, 146(1):100-119. DOI URL
[52]	BURNHAM C W, DAVIS N F. The role of H₂O in silicate melts: Si₃O₈-H₂O to 10 kilobars and 700-1 000 ℃[J]. American Journal of Science, 1974, 274:902-940. DOI URL
[53]	LONDON D. Internal differentiation of rare-element pegmatites: effects of boron, phosphorus, and fluorine[J]. Geochimica et Cosmochimica Acta, 1987, 51(3):403-420. DOI URL
[54]	LONDON D, MORGAN G B, BABB H A, et al. Behavior and effects of phosphorus in the system Na₂O-K₂O-Al₂O₃-SiO₂-P₂O₅-H₂O at 200 MPa(H₂O)[J]. Contributions to Mineralogy and Petrology, 1993, 113(4):450-465. DOI URL
[55]	BORCHERT M, WILKE M, SCHMIDT C, et al. Partitioning of Ba, La, Yb and Y between haplogranitic melts and aqueous solutions: an experimental study[J]. Chemical Geology, 2010, 276(3/4):225-240. DOI URL
[56]	HU X Y, BI X W, SHANG L B, et al. An experimental study of tin partition between melt and aqueous fluid in F/Cl-coexisting magma[J]. Chinese Science Bulletin, 2009, 54(6):1087-1097.
[57]	ČERNÝ P. Characteristics of pegmatite deposits of tantalum[M]// Lanthanides, tantalum and niobium. Berlin: Springer-Verlag, 1989: 195-239.
[58]	PARTINGTON G A, MCNAUGHTON N J, WILLIAMS I S. A review of the geology, mineralization, and geochronology of the Greenbushes Pegmatite, Western Australia[J]. Economic Geology, 1995, 90(3):616-635. DOI URL
[59]	ČERNÝ P. The Tanco rare-element pegmatite deposit, Manitoba: regional context, internal anatomy, and global comparisons[M]// Rare-element geochemistry of ore deposits. St John’s: Geological Association of Canada, 2005: 127-158.
[60]	RAO C, WANG R C, HU H, et al. Complex internal textures in oxide minerals from the Nanping No.31 dyke of granitic pegmatite, Fujian Province, Southeastern China[J]. The Canadian Mineralogist, 2009, 47(5):1195-1212. DOI URL
[61]	BREITER K, KORBELOVÁ Z, CHLÁDEK S, et al. Diversity of Ti-Sn-W-Nb-Ta oxide minerals in the classic granite-related magmatic-hydrothermal Cínovec/Zinnwald Sn-W-Li deposit (Czech Republic)[J]. European Journal of Mineralogy, 2017, 29(4):727-738. DOI URL
[62]	WU M Q, SAMSON I M, ZHANG D H. Textural and chemical constraints on the formation of disseminated granite-hosted W-Ta-Nb mineralization at the Dajishan deposit, Nanling Range, Southeastern China[J]. Economic Geology, 2017, 112(4):855-887. DOI URL
[63]	WU M Q, SAMSON I M, ZHANG D H. Textural features and chemical evolution in Ta-Nb oxides: implications for deuteric rare-metal mineralization in the Yichun Granite-Marginal Pegmatite, Southeastern China[J]. Economic Geology, 2018, 113(4):937-960. DOI URL
[64]	VAN LICHTERVELDE M, BEZIAT D, SALVI S, et al. Textures and chemical evolutions in tantalum oxides: a discussion of magmatic versus metasomatic origins for Ta mineralization in the Tanco Lower Pegmatite, Manitoba, Canada[J]. Economic Geology, 2007, 102(2):257-276. DOI URL
[65]	MCNEIL A G, LINNEN R L, FLEMMING R L, et al. An experimental approach to examine fluid-melt interaction and mineralization in rare-metal pegmatites[J]. American Mineralogist, 2020, 105(7):1078-1087. DOI URL
[66]	LONDON D. Geochemistry of alkalis and alkaline earths in ore-forming granites, pegmatites, and rhyolites[M]// Rare-element geochemistry of ore deposits. St John’s: Geological Association of Canada, 2005: 17-43.
[67]	LINNEN R L, CUNEY M. Granite-related rare-element deposits and experimental constraints on Ta-Nb-W-Sn-Zr-Hf mineralization[M]// Rare-element geochemistry and mineral deposits. St John’s: Geological Association of Canada, 2005: 45-67.
[68]	王汝成, 谢磊, 诸泽颖, 等. 云母:花岗岩-伟晶岩稀有金属成矿作用的重要标志矿物[J]. 岩石学报, 2019, 35(1):69-75.
[69]	BREITER K, VANKOVÁ M, GALIOVÁ M V, et al. Lithium and trace-element concentrations in trioctahedral micas from granites of different geochemical types measured via laser ablation ICP-MS[J]. Mineralogical Magazine, 2017, 81(1):15-33. DOI URL
[70]	LI J, HUANG X L, HE P L, et al. In situ analyses of micas in the Yashan granite, South China: constraints on magmatic and hydrothermal evolutions of W and Ta-Nb bearing granites[J]. Ore Geology Reviews, 2015, 65:793-810. DOI URL
[71]	LONDON D. Pegmatite[M]. Quebec: Mineralogical Association of Canada, 2018.

稀有金属矿物溶解度对花岗伟晶岩成矿作用的制约

Solubility of rare metals as a constraint on mineralization of granitic pegmatite

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