Zhu J C;Wu C N;Liu C S;Li F C,Huang X L and Zhou D S.Magmatic-hydrothermal evolution and genesis of Koktokay No.3rare metal pegmatite dyke,Altai,China[J].Geological Journal of China Universities,2000(1)
[4]
ZhangD H;XuJ H;Yu X Q;Li J K Mao S D and Li Y Q.The diagentiec and metalloginic depth:Main constrains and the estimation methods (in Chinese with Englishi abstrcat)[J].Geological Bulletin of China,2011(1)
[5]
Zhang D H;Zhang W H;Xu G J.Exsolution and evolution of magmatic hydrothermal fluids and their constraints on the porphyry ore-forming system (in Chinese with Englishi abstrcat)[J].Earthquake Science Frontiers,2001(3)
[6]
Zajacz Z;Halter W E;Pettke T;Guillong M,Determination of fluid/melt partition coefficients by LA-ICPMS analysis of co-existing fluid and silicate melt inclusions:Controls on element partitioning,Geochimica et Cosmochimica Acta,2008.
[7]
Johannes W,Beginning of melting in the granite system Qz-Or-Ab-H2O,Contributions to Mineralogy & Petrology,1984.
[8]
Jahns R H,Internal evolution of pegmatite bodies,1982.
[9]
Huang H L;Chang H L;Fu J M;Wang X W and Li T Y.Formation pressure of wolframite-vein deposits and emplacement depth of related granite in Xihuashan,Jiangxi Province (in Chinese with Englishi abstrcat)[J].Mineral Deposits,2006(5)
[10]
Thomas R;Webster J D;Rhede D,The transition from peraluminous to peralkaline granite melts:Evidence from melt inclusions and accessory minerals,Lithos,2006.
[11]
Thomas R;Webster J D,Strong tin enrichment in a pegmatite-forming melt,Mineral Deposits,2000.
[12]
Student J J;Bodnar R J,Synthetic fluid inclusions XIV:Coexisting silicate melt and aqueous fluid inclusions in the Haplogranite-H2O-NaCl-KCl system,Journal of Peterology,1999.
[13]
Student J J;Bodnar R J,Melt inclusion microthermometry:Petrologic constraints from the H2O-saturated haplogranite system,Petrology,1996.
[14]
Snelling A A,Catastrophic granite formation:Rapid melting of source rocks,and rapid magma Intrusion and Cooling,Answers Research Journal,2008(1).
[15]
London D,Formation of tourmaline-rich gem pockets in miarolitic pegmatites,American Mineralogist,1986.
[16]
ANDREAS AUDETAT ；THOMAS PETTKE ；CHRISTOPH A. HEINRICH,The Composition of Magmatic-Hydrothermal Fluids in Barren and Mineralized Intrusions,Economic geology？,2008, 103(5).
[17]
London D,The magmatic-hydrothermal transition in the Tanco rare-element pegmatite:Evidence from fluid inclusions and phase equilibrium experiments,American Mineralogist,1986.
[18]
London D,Experimental phase equilibria in the system LiAlSiO4-SiO2-H2O:A petrogenetic grid for lithiumrich pegmatites,American Mineralogist,1984.
[19]
Li J K;Chou I-Ming;Yuan S D;Burruss R C,Homogenization temperature measurements in hydrothermal diamond-anvil cell for melt and fluid incluisons from the Jiajika pegmatite deposit,China,EOS(Transactions of the American Geophysical Union),2009(52).
[20]
Li J K,Mineralization mechanism and continental geodynamics of pegmatite type depsoits in western Sichuan,China,北京:原子能出版社,2007.
[21]
Candela P A,A review of shallow,ore-related granites:Textures,volatiles,and ore metals,Journal of Petrology,1997(12).
[22]
Frezzotti M L,Silicate-melt inclusions in magmatic rocks:Applications to petrology,Lithos,2001.
[23]
Darling R S;Bassett W,Analysis of natural H2O + CO2 + NaCl fluid inclusions in the hydrothermal diamond anvil cell,American Mineralogist,2002.
[24]
Chou I M.Hydrothermal diamond-anvil cell:Application to studies of geologic fluids (in Englishi with Chinese abstract)[J].Acta Petrologica Sinica,2003(2)
Lowenstern J B,Applications of silicate melt inclusions to the study of magmatic volatiles,1995.
[28]
London D,The origin of primary textures in granitic pegmatites,The Canadian Mineralogist,2009.
[29]
Yang K;Bodnar R J,Magmatic-hydrothermal evolution in the bottoms of porphyry copper systems:Evidence from the silicate melt and aqueous fluid inclusions in the Gyeongsang Basin,South Korea,International Geology Review,1994.
[30]
Webster J D;Thomas R,Silicate melt inclusion in felsic plutons:A synthesis and review,2006.
[31]
Candela P A;Piccoli P M,Model ore-metal partitioning from melts into vapor and vapor/brine mixtures,Mineralogical Association of Canada Short Course,1995.
[32]
Watson E.B;Harrison T.M,Zircon saturation revisited:Temperature and composition effects in a variety of crustal magma types,Earth and Planetary Science Letters？ ,1983, 64.
[33]
Walker T,Granite grain size:Not a problem for rapid cooling of plutons,Journal of Creation,2003(2).
[34]
Thomas R;Davidson P;Badanina E,A melt and fluid inclusion assemblage in beryl from pegmatite in the Orlovka amazonite granite,East Transbaikalia,Russia:Implications for pegmatiteforming melt systems,Mineralogy and Petrology,2009.
[35]
Portnyagin M V;Plechov P Y;Osipenko A B,Influence of natural decrepitation on the composition of melt inclusions in olivine:A study of melanocratic basalts from Avacha volcano,Kamchatka,Experiment in GeoSciences,2000(1).
[36]
Nakano T;Urabe T,Calculated compositions of fluids released from a crystallizing granitic melt:Importance of pressure on the genesis of ore forming fluid,Geochemical Journal,1989.
[37]
Nabelek P I;Whittington A G;Sirbescu M C,The role of H2O in rapid emplacement and crystallization of granite pegmatites:Resolving the paradox of large crystals in highly under cooled melts,Contributions to Mineralogy & Petrology,2009.
[38]
Miller C F;McDowell S M;Mapes R W,Hot and cold granites? Implications of zircon saturation temperatures and preservation of inheritance,Geology,2004(6).
[39]
Manning D A,The effect of fluorine on liquidus phase relationships in the system Qz-Ab-Or with excess water at 1kb,Contributions to Mineralogy & Petrology,1981.
[40]
更多...
[41]
Lu H Z;Wang Z G;Li Y S,Magma/fluid transition and genesis of pegmatite di 3 at Altay,Xinjiang,Acta Mineralogica Sinica,1996(1).
Schtnidt C;Chou I-Ming;Bodnar R J;Bassett W A,Microthermometric analysis of synthetic fluid inclusions in the hydrothermal diamond-anvil cell,American Mineralogist,1998.
Bassett W A;Shen A H;Bucknum M;Chou I-Ming,A new diamond anvil cell for hydrothermal studies to 2.5 GPa and from 190 to 1200℃,Review of Scientific Instruments,1993.
[48]
Hossain I;Tsunogae T,Fluid inclusion study of pegmatite and aplite veins of palaeoproterozoic basement rocks in Bangladesh:Implication for magmatic fluid compositions and crystallization depth,JOURNAL OF MINERALOGICAL AND PETROLOGICAL SCIENCES,2008(2).
[49]
Holtz F;Pichavant M;Barbey P;JohannesW,Effects of H2O on liquidus phase relations in the haplogranite system at 2 and 5 kbar,American Mineralogist,1992.
[50]
Hanley, JJ ；Mungall, JE ；Pettke, T ；Spooner, ETC ；Bray, CJ,Fluid and halide melt inclusions of magmatic origin in the ultramafic and lower banded series, Stillwater Complex, Montana, USA,Journal of Petrology？,2008, 49(6).
[51]
Anderson A J;Clark A H;Gray S,The occurrence and origin of zabuyelite (Li2CO3) in spodumene-hosted fluid inclusions:implications for the internal evolution of rare-element granitic pegmatites,The Canadian Mineralogist,2001(6).
[52]
London D,Pegmatites,The Canadian Mineralogist,Special Publication,2008.
