峨眉山大火成岩省的岩浆运移、滞留、演化过程的岩石学和数值模拟研究
|
摘要
按早期玄武岩→辉长岩→晚期酸性岩的时间顺序，探讨了峨眉山大火成岩省幔源岩浆在地壳运移，滞留和演化的过程。通过结合这些方法，可以全面认识岩浆过程中的五个主要变量即时间，空间，温度，压力和成分，从而更准确地揭示峨眉山大火成岩省中的岩浆作用的化学过程和物理过程。论文取得以下主要的成果和认识：
基于前人提出的地幔熔融柱模型和反演方法笔者编写了一个界面友好的应用软件Calmantle1.0。应用Calmantle1.0，用户可轻易获得玄武岩部分熔融源区的起止条件包括温度，压力，深度和部分熔融程度。
将大桥剖面出露的斜长石巨晶玄武岩细分为离散型（SI型）和聚集型（CT型）。两种斜长石巨晶玄武岩全岩成分上都显示出低MgO，高Ti和高FeO特征。两类斜长石巨晶在定量化结构图上都表现出S型CSD特征，但是存在明显不同的特征长度。假设斜长石巨晶的生长速率为10-11-10-10mm/s,那么CT型和SI型的斜长石巨晶的生长时间分别为500–6,000年和1,000–10,000年。我们给出一个新的再活化基质，即流体的注入导致岩浆黏度的急剧下降从而使得滞留岩浆再活化并且快速喷出。Sr-Nd-Pb相关图解指示峨眉山低Mg斜长石巨晶玄武岩靠近EMI区域。
攀枝花铁矿区斜长石巨晶辉长岩以岩墙形式侵入到了其底带的细粒辉长岩。斜长石巨晶从核部到边部的原位Sr同位素成分剖面较为稳定，表明斜长石巨晶不是循环晶。斜长石巨晶辉长岩在CSD图解上呈线性，取斜长石巨晶的生长速率为10-11-10-10mm/s,那么其生长时间为530-8118年。假设对于100km3岩浆房，以1000MW的功率散热,达到50%晶体含量，辉长岩体需要～2400年。巨晶生长时间和数值模拟约束攀枝花侵入体的侵位时间和冷却时间发生在千年尺度。
通过对大老包黑云母二长花岗岩的锆石LA-ICP-MSU-Pb年龄测定，获得大老包花岗岩形成时代为257.1±1.7Ma。基于下地壳热区模型进行数值模拟结果，认为大老包花岗岩可能是峨眉山大火成岩省中底侵的玄武质岩浆在3Ma内部分熔融下地壳形成的。
Based on the field work, quantitative textural analysis theory and geochemistry, we studied the magma transfer, storage and evolution by studying basalts, grabbros and granites in Emeishan large igneous province(LIP) in this PhD dissertation. Using these methods, we kwon the five basic variables of time, space, temperature, pressure and composition, and as far as seeks to clarify the magma chemical and physical process. The dissertation made several major achievements and insights as follows:
Based on the proposed previously mantle melting column model and its inversion method, we have designed an implication software Calmantle1.0with friend interfaces. Using this software, users can easily obtain the partial melting conditions at the initial and final stages, including temperature, pressure, depth, the degree of partial melting and so on.
We report a quantitative textural analysis and bulk-rock geochemical composition of clustered touching crystals (CT-type) and single isolated crystal (SI-type) GPB samples in the Daqiao section. Both types of GPBs are evolved, but have high Ti/Y ratiosand high total FeO content. The two types of GPBs have S-type crystal size distributions but have quite different characteristic lengths. For plagioclase growth rates of10-11to10-10mm/s, The plagioclase megacrysts have the residence time of about500-6,000years, about1,000-10,000years, respectively. We suggest that CT-and SI-type crystals grew and were coarsened in the outer part and inner part of a magma chamber, respectively. Magma evolution during storage is controlled by crystallization, crystal growth, and magma mixing, and pulsating eruptions occur in response to the continuous supply of hot magma and fluid intrusions. The isotopic compositions show they are from EM I.
The giant plagioclase gabbros (GPG) dykes mostly intrude into the fine-grained gabbros without significant contact. However, the mineral composition results show that most of the plagioclase megacrysts contain less An than do plagioclase in fine-grained gabbro samples. In situ analyses of Sr isotopes from core-to-rim transects of plagioclase megacrysts are constant, indicating there are no recycling crystals. For a plagioclase growth range of10-11-10-10mm/s, the plagioclase should have a growth time of530-8118years. In a100km3magma chamber releasing thermal energy at a rate of1000MW, Panzhihua intrusion should reach50%crystallization after -2400years. The growth time recorded by the megacrysts in GPG and numerical modelling may constrain the emplacement timescales of Panzhihua intrusion may take place on thousands of years.
The Hongge Dalaobao granitic stock in the Emeishan large igneous province, SW China. In situ ziron LA-ICP-MS U-Pb age indicates that the age of monzogranite is257.1±1.7Ma. Based on the deep crustal hot zones, the results of numerical simulation show that the partial melting of deep crust and the Dalaobao granites magmatism are triggered by conductive heating of the mantle-driven magma within3Ma.
基于前人提出的地幔熔融柱模型和反演方法笔者编写了一个界面友好的应用软件Calmantle1.0。应用Calmantle1.0，用户可轻易获得玄武岩部分熔融源区的起止条件包括温度，压力，深度和部分熔融程度。
将大桥剖面出露的斜长石巨晶玄武岩细分为离散型（SI型）和聚集型（CT型）。两种斜长石巨晶玄武岩全岩成分上都显示出低MgO，高Ti和高FeO特征。两类斜长石巨晶在定量化结构图上都表现出S型CSD特征，但是存在明显不同的特征长度。假设斜长石巨晶的生长速率为10-11-10-10mm/s,那么CT型和SI型的斜长石巨晶的生长时间分别为500–6,000年和1,000–10,000年。我们给出一个新的再活化基质，即流体的注入导致岩浆黏度的急剧下降从而使得滞留岩浆再活化并且快速喷出。Sr-Nd-Pb相关图解指示峨眉山低Mg斜长石巨晶玄武岩靠近EMI区域。
攀枝花铁矿区斜长石巨晶辉长岩以岩墙形式侵入到了其底带的细粒辉长岩。斜长石巨晶从核部到边部的原位Sr同位素成分剖面较为稳定，表明斜长石巨晶不是循环晶。斜长石巨晶辉长岩在CSD图解上呈线性，取斜长石巨晶的生长速率为10-11-10-10mm/s,那么其生长时间为530-8118年。假设对于100km3岩浆房，以1000MW的功率散热,达到50%晶体含量，辉长岩体需要～2400年。巨晶生长时间和数值模拟约束攀枝花侵入体的侵位时间和冷却时间发生在千年尺度。
通过对大老包黑云母二长花岗岩的锆石LA-ICP-MSU-Pb年龄测定，获得大老包花岗岩形成时代为257.1±1.7Ma。基于下地壳热区模型进行数值模拟结果，认为大老包花岗岩可能是峨眉山大火成岩省中底侵的玄武质岩浆在3Ma内部分熔融下地壳形成的。
Based on the field work, quantitative textural analysis theory and geochemistry, we studied the magma transfer, storage and evolution by studying basalts, grabbros and granites in Emeishan large igneous province(LIP) in this PhD dissertation. Using these methods, we kwon the five basic variables of time, space, temperature, pressure and composition, and as far as seeks to clarify the magma chemical and physical process. The dissertation made several major achievements and insights as follows:
Based on the proposed previously mantle melting column model and its inversion method, we have designed an implication software Calmantle1.0with friend interfaces. Using this software, users can easily obtain the partial melting conditions at the initial and final stages, including temperature, pressure, depth, the degree of partial melting and so on.
We report a quantitative textural analysis and bulk-rock geochemical composition of clustered touching crystals (CT-type) and single isolated crystal (SI-type) GPB samples in the Daqiao section. Both types of GPBs are evolved, but have high Ti/Y ratiosand high total FeO content. The two types of GPBs have S-type crystal size distributions but have quite different characteristic lengths. For plagioclase growth rates of10-11to10-10mm/s, The plagioclase megacrysts have the residence time of about500-6,000years, about1,000-10,000years, respectively. We suggest that CT-and SI-type crystals grew and were coarsened in the outer part and inner part of a magma chamber, respectively. Magma evolution during storage is controlled by crystallization, crystal growth, and magma mixing, and pulsating eruptions occur in response to the continuous supply of hot magma and fluid intrusions. The isotopic compositions show they are from EM I.
The giant plagioclase gabbros (GPG) dykes mostly intrude into the fine-grained gabbros without significant contact. However, the mineral composition results show that most of the plagioclase megacrysts contain less An than do plagioclase in fine-grained gabbro samples. In situ analyses of Sr isotopes from core-to-rim transects of plagioclase megacrysts are constant, indicating there are no recycling crystals. For a plagioclase growth range of10-11-10-10mm/s, the plagioclase should have a growth time of530-8118years. In a100km3magma chamber releasing thermal energy at a rate of1000MW, Panzhihua intrusion should reach50%crystallization after -2400years. The growth time recorded by the megacrysts in GPG and numerical modelling may constrain the emplacement timescales of Panzhihua intrusion may take place on thousands of years.
The Hongge Dalaobao granitic stock in the Emeishan large igneous province, SW China. In situ ziron LA-ICP-MS U-Pb age indicates that the age of monzogranite is257.1±1.7Ma. Based on the deep crustal hot zones, the results of numerical simulation show that the partial melting of deep crust and the Dalaobao granites magmatism are triggered by conductive heating of the mantle-driven magma within3Ma.
引文
Acosta-Vigil, A., London, D., Morgan, G.B., Experiments on the kinetics of partial melting of a leucogranite at200MPa H2O and690-800℃:compositional variability of melts during the onset of H2O-saturated crustal anatexis. Contrib Mineral Petrol,151:539-557
Ali, J.R., Lo, C.H., Thompson, G.M. and Song, X.,2004. Emeishan Basalt Ar-Ar overprint ages define several tectonic events that affected the western Yangtze platform in the Mesozoic and Cenozoic. Journal of Asian Earth Sciences,23(2):163-178.
Ali, J.R., Thompson, G.M., Zhou, M.F. and Song, X.,2005. Emeishan large igneous province, SW China. Lithos,79(3-4):475-489.
Anderson, D.L.,2005. Large Igneous Provinces, Delamination, and Fertile Mantle. Elements,1(5):271-275.
Annen, C, Blundy, J.D. and Sparks, R.S.J.,2006. The Genesis of Intermediate and Silicic Magmas in Deep Crustal Hot Zones. Journal of Petrology,47(3):505-539.
Armienti, P., Perinelli, C. and Putirka, K.D.,2012. A New Model to Estimate Deep-level Magma Ascent Rates, with Applications to Mt. Etna (Sicily, Italy). Journal of Petrology.
Arndt, N., Chauvel, C, Czamanske, G. and Fedorenko, V.,1998. Two mantle sources, two plumbing systems:tholeiitic and alkaline magmatism of the Maymecha River basin, Siberian flood volcanic province. Contributions to Mineralogy and Petrology,133(3):297-313.
Bachmann, O. and Bergantz, G.W.,2003. Rejuvenation of the Fish Canyonmagma body:a window into the evolution of large-volume silicic magma systems. Geology,31:789-792.
Bachmann, O. and Bergantz, G.,2006. Gaspercolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies, Journal of Volcanology and Geothermal research,149:85-102
Bachmann, O., Michael, A.D. and Peter, W.L.,2002. The fish canyon magma body,san juan volcanic field, colorado:rejuvenation and eruption of an upper-crustal batholith. Journal of petrology.23:1469-1503
Beane, J.E., Turner, C.A., Hooper, P.R., Subbarao, K.V. and Walsh, J.N.,1986. Stratigraphy, composition and form of the Deccan Basalts, Western Ghats, India. Bulletin of Volcanology,48(1):61-83.
Blundy, J. and Cashman, K.,2001. Ascent-driven crystallisation of dacite magmas at Mount St Helens,1980-1986. Contrib Mineral Petrol,140:631-650
Boorman, S., Boudreau, A. and Kruger, F.J.,2004. The Lower Zone-Critical Zone Transition of the Bushveld Complex:a Quantitative Textural Study. Journal of Petrology,45(6):1209-1235.
Bryan, S.E. and Ernst, R.E.,2008. Revised definition of Large Igneous Provinces (LIPs). Earth-Science Reviews,86(1-4):175-202.
Bryan, S.E., Peate, I.U., Peate, D.W., Self, S., Jerram, D.A., Mawby, M.R., Marsh, J.S. and Miller, J.A.,2010. The largest volcanic eruptions on Earth. Earth-Science Reviews,102(3-4):207-229.
Burgisser, A. and Bergantz, G.W.,2011. A rapid mechanism to remobilize and homogenize highly crystalline magma bodies. Nature,471:212-215
Campbell, I,H, and Turnerm J.S.,1985. Turbulent mixing between fluids with different viscosities.Nature,313:39-42
Campbell, I.H. and Turner, J.S.,1986. The influence of viscosity on fountains in magma chambers. J.Petrology,27:1-30
Cashman, K.V.,1993. Relationship between plagioclase crystallization and cooling rate in basaltic melts. Contributions to Mineralogy and Petrology,113(1):126-142.
Cashman, K.V. and Marsh, B.D.,1988. Crystal size distribution (CSD) in rocks and the kinetics and dynamics of crystallization II:Makaopuhi lava lake. Contributions to Mineralogy and Petrology,99(3):292-305.
Chandrasekharam, D., Mahoney, J.J., Sheth, H.C. and Duncan, R.A.,1999. Elemental and Nd-Sr-Pb isotope geochemistry of flows and dikes from the Tapi rift, Deccan flood basalt province, India. Journal of Volcanology and Geothermal Research,93(1-2):111-123.
Cheikh, N.D., Beya, B.B. and Lili, T.2007. Natural convection flow in a tall enclosure using a multigrid method. C.R.Mecanique.335,113-118
Cheng, L.L., Yang, Z.F., Zeng, L., Wang, Y. and Luo, Z.H.,2014. Giant plagioclase growth during storage of basaltic magma in Emeishan Large Igneous Province, SW China. Contributions to Mineralogy and Petrology,167(2):1-20.
Chung, S.L. and Jahn, B.M.,1995. Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary. Geology,23(10):889-892.
Chung, S.L., Jahn, B., Genyao, W., Lo, C.H. and Bolin, C.,1998. The Emeishan flood basalt in SW China:A mantle plume initiation model and its connection with continental breakup and mass extinction at the Permian-Triassic Boundary, Mantle Dynamics and Plate Interactions in East Asia. Geodyn. Ser. AGU, Washington, DC, pp.47-58.
Coffin, M.F. and Eldholm,O.,1994. Large igneous provinces:crustal structure, dimensions, and external consequences. Reviews of Geophysics,32(1):1-36.
Couch, S., Sparks, R.S.J. and Carroll, M.R.,2001. Mineral disequilibrium in lavas explained by convective self-mixing in open magma chambers. Nature,411:1037-1039
Couch, S., Sparks, R.S.J. and Carroll, M.R.,2003. The Kinetics of Degassing-Induced Crystallization at Soufriere Hills Volcano, Montserrat. Journal of Petrology,44(8):1477-1502.
Cordier, C, Caroff, M. and Rannou, E.,2012. Timescale of open-reservoir evolution beneath the south Cleft segment, Juan de Fuca ridge. Mineralogy and Petrology,104(1-2):1-14.
Cox, K.G.,1980. A Model for Flood Basalt Vulcanism. Journal of Petrology,21(4):629-650.
Cox, K.G.M., R.; Hornung G.,1967. Geochemical and petrographic provinces in the Karoo basalts of southern Africa. American Mineralogist,52:1451-1474.
DeHoff, R.T.,1991. A geometrically general theory of diffusion controlled coarsening. Acta Metallurgica et Materialia,39(10):2349-2360.
Dong, H., Xing, C. and Wang, C.Y.,2013. Textures and mineral compositions of the Xinjie layered intrusion, SW China:Implications for the origin of magnetite and fractionation process of Fe-Ti-rich basaltic magmas. Geoscience Frontiers,4(5):503-515.
Elburg, M., Vroon, P., van der Wagt, B. and Tchalikian, A.,2005. Sr and Pb isotopic composition of five USGS glasses (BHVO-2G, BIR-1G, BCR-2G, TB-1G, NKT-1G). Chemical Geology,223(4):196-207.
Ernst, R.E., Buchan, K.L. and Campbell, I.H.,2005. Frontiers in large igneous province research. Lithos,79(3-4):271-297.
Ewart, A., Marsh, J.S., Milner, S.C., Duncan, A.R., Kamber, B.S. and Armstrong, R.A.,2004. Petrology and Geochemistry of Early Cretaceous Bimodal Continental Flood Volcanism of the NW Etendeka, Namibia. Part1:Introduction, Mafic Lavas and Re-evaluation of Mantle Source Components. Journal of Petrology,45(1):59-105.
Ewart, A., Milner, S.C., Armstrong, R.A. and Dungan, A.R.,1998. Etendeka Volcanism of the Goboboseb Mountains and Messum Igneous Complex, Namibia. Part I:Geochemical Evidence of Early Cretaceous Tristan Plume Melts and the Role of Crustal Contamination in the Parana-Etendeka CFB. Journal of Petrology,39(2):191-225.
Fan, W., Zhang, C, Wang, Y., Guo, F. and Peng, T.,2008. Geochronology and geochemistry of Permian basalts in western Guangxi Province, Southwest China:Evidence for plume-lithosphere interaction. Lithos,102(1-2):218-236.
Freysteinn et al (2010) Freysteinn S et al.2010. Intrusion triggering of the2010Eyjafjallajokull explosive eruption. Nature.468:426-430
Ganino, C, Arndt, N., Zhou, M.-F, Gaillard, F. and Chauvel, C.,2008. Interaction of magma with sedimentary wall rock and magnetite ore genesis in the Panzhihua mafic intrusion, SW China. Miner Deposita,43(6):677-694.
Ghiorso, M. and Sack, R.,1995. Chemical mass transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures. Contributions to Mineralogy and Petrology,119(2-3):197-212.
Griffiths, R.W. and Campbell, I.H.,1990. Stirring and structure in mantle starting plumes. Earth and Planetary Science Letters,99(1):66-78.
Hanski, E., Kamenetsky, V.S., Luo, Z.-Y., Xu, Y.-G. and Kuzmin, D.V.,2010. Primitive magmas in the Emeishan Large Igneous Province, southwestern China and northern Vietnam. Lithos,119(1-2):75-90.
He, B., Xu, Y. and Campbell, I.,2009. Pre-eruptive uplift in the Emeishan? Nature Geosci,2(8):530-531.
He, B., Xu, Y.G., Chung, S.L., Xiao, L. and Wang, Y.,2003. Sedimentary evidence for a rapid, kilometer-scale crustal doming prior to the eruption of the Emeishan flood basalts. Earth and Planetary Science Letters,213(3-4):391-405.
He, B., Xu, Y.G., Huang, X.L., Luo, Z.Y., Shi, Y.R., Yang, Q.J. and Yu, S.Y.,2007. Age and duration of the Emeishan flood volcanism, SW China:Geochemistry and SHRIMP zircon U-Pb dating of silicic ignimbrites, post-volcanic Xuanwei Formation and clay tuff at the Chaotian section. Earth and Planetary Science Letters,255(3-4):306-323.
Higgins, M.D.,1994. Determination of crystal morphology and size from bulk measurements on thin sections:numerical modelling. American Mineralogist,79:113-119.
Higgins, M.D.,1996. Magma dynamics beneath Kameni volcano, Thera, Greece, as revealed by crystal size and shape measurements. Journal of Volcanology and Geothermal Research,70(1-2):37-48.
Higgins, M.D.,1998. Origin of Anorthosite by Textural Coarsening:Quantitative Measurements of a Natural Sequence of Textural Development. Journal of Petrology,39(7):1307-1323.
Higgins, M.D.,2000. Measurement of crystal size distributions. American Mineralogist,85(9):1105-1116.
Higgins, M.D.,2006. Verification of ideal semi-logarithmic, lognormal or fractal crystal size distributions from2D datasets. Journal of Volcanology and Geothermal Research,154:8-16.
Higgins, M.D.,2009. The Cascadia megathrust earthquake of1700may have rejuvenated an isolated basalt volcano in western Canada:Age and petrographic evidence. Journal of Volcanology and Geothermal Research,179(1-2):149-156.
Higgins, M.D.,2011a. Quantitative petrological evidence for the origin of K-feldspar megacrysts in dacites from Taapaca volcano, Chile. Contributions to Mineralogy and Petrology,162(4):709-723.
Higgins, M.D.,2011b. Textural coarsening in igneous rocks. International Geology Review,53(3-4):354-376.Higgins, M.D. and Chandrasekharam, D.,2007. Nature of Sub-volcanic Magma Chambers, Deccan Province, India:Evidence from Quantitative Textural Analysis of Plagioclase Megacrysts in the Giant Plagioclase Basalts. Journal of Petrology,48(5):885-900.
Hildreth W.2007. Quaternary Magmatism in the Cascades:Geo-logical Perspectives[M]. USGS Professional Paper,1744:1-125.
Hooper, P.R.,1997. The Columbia River flood basalt province:Current status, Large Igneous Provinces:Continental, Oceanic, and Planetary Flood Volcanism. Geophys. Monogr. Ser. AGU, Washington, DC, pp.1-27.
Hooper, P.R., Subbarao, K.V. and Beane, J.E.,1988. The giant plagioclase basalts (GPBs) of the western Ghats, Deccan Traps. Geological Society of India Memoir,10:135-144.
Hossain, M.A. and Wilson,M.2002. Natural convection flow in a fluid-saturated porous medium enclosed by non-isothermal walls with heat generation.Int. J.Therm.Sci.41,447-454
Hou, T., Zhang, Z., Encarnacion, J., Santosh, M. and Sun, Y.,2013. The role of recycled oceanic crust in magmatism and metallogeny:Os-Sr-Nd isotopes, U-Pb geochronology and geochemistry of picritic dykes in the Panzhihua giant Fe-Ti oxide deposit, central Emeishan large igneous province, SW China. Contributions to Mineralogy and Petrology,165(4):805-822.
Hou, T., Zhang, Z., Kusky, T., Du, Y., Liu, J. and Zhao, Z.,2011. A reappraisal of the high-Ti and low-Ti classification of basalts and petrogenetic linkage between basalts and mafic-ultramafic intrusions in the Emeishan Large Igneous Province, SW China. Ore Geology Reviews,41(1):133-143.
Howarth, G.H. and Prevec, S.A.,2013. Hydration vs. oxidation:Modelling implications for Fe-Ti oxide crystallisation in mafic intrusions, with specific reference to the Panzhihua intrusion, SW China. Geoscience Frontiers,4(5):555-569.
Huber, C, Bachmann, O. and Dufek, J.,2010. The limitations of melting on the reactivation of silicic mushes. J. Volcanol. Geotherm. Res.,195:97-105
Hummel, W. and Arndt, J.,1985. Variation of viscosity with temperature and composition in the plagioclase system. Contrib Mineral Petrol,90:83-92
Huppert, H.E. and Sparks, R.S.J.,1988. The generation of granitic magmas by intrusion of basalt into continental crust. J. Petrol,29:599-624
Irvine, T.N.,1975. Crystallization sequences in the Muskox intrusion and other layered intrusions—Ⅱ. Origin of chromitite layers and similar deposits of other magmatic ores. Geochimica et Cosmochimica Acta,39(6-7):991-1020.
Jerram, D.A. and Martin, V.M.,2008. Understanding crystal populations and their significance through the magma plumbing system. Geological Society, London, Special Publications,304(1):133-148.
Kamenetsky, V.S., Chung, S.L., Kamenetsky, M.B. and Kuzmin, D.V.,2012. Picrites from the Emeishan Large Igneous Province, SW China:a Compositional Continuum in Primitive Magmas and their Respective Mantle Sources. Journal of Petrology,53(10):2095-2113.
Lange, R.A., Frey, H.M. and Hector, J.,2009. A thermodynamic model for the plagioclase-liquid hygrometer/thermometer. American Mineralogist,94(4):494-506.
Langmuir, C.H., Klein, E.M. and Plank, T.,1992. Petrological systematics of mid-ocean ridge basalts:Constraints on melt generation beneath ocean ridges. Geophysical Monograph Series,71:183-280.
Lai, S., Qin, J., Li, Y., Li, S. and Santosh, M.,2012. Permian high Ti/Y basalts from the eastern part of the Emeishan Large Igneous Province, southwestern China:Petrogenesis and tectonic implications. Journal of Asian Earth Sciences,47(0):216-230.
Larsen, L.M. and Pedersen, A.K.,2000. Processes in high-Mg, high-T magmas:evidence from olivine, chromite and glass in Palaeogene picrites from West Greenland. Journal of Petrology,41(7):1071-1098.
Li, C, Tao, Y., Qi, L. and Ripley, E.M.,2012. Controls on PGE fractionation in the Emeishan picrites and basalts:Constraints from integrated lithophile-siderophile elements and Sr-Nd isotopes. Geochimica et Cosmochimica Acta,90(0):12-32.
Lifshitz, I.M. and Slyozov, V.V.,1961. The kinetics of precipitation from supersaturated solid solutions. Journal of Physics and Chemistry of Solids,19(1-2):35-50.
Lightfoot, P.C., Hawkesworth, C.J., Hergt, J., Naldrett, A.J., Gorbachev, N.S., Fedorenko, V.A. and Doherty, W.,1993. Remobilisation of the continental lithosphere by a mantle plume: major-, trace-element, and Sr-, Nd-, and Pb-isotope evidence from picritic and tholeiitic lavas of the Noril'sk District, Siberian Trap, Russia. Contributions to Mineralogy and Petrology,114(2):171-188.
Li, Y.G., Ma, Y, Ji, X., Li, J., Huang, M. and Min, Z.,2003. Mineral resources of Panzhihua, Sichuan Province, S W China. Chengdu University of Technology,275.
Lo, C.H., Chung, S.L., Lee, T.Y. and Wu, G,2002. Age of the Emeishan flood magmatism and relations to Permian-Triassic boundary events. Earth and Planetary Science Letters,198(3):449-458.
Magee, C, O'driscoll, B. and Chambers, A.D.,2010. Crystallization and textural evolution of a closed-system magma chamber:insights from a crystal size distribution study of the Lilloise layered intrusion, East Greenland. Geological Magazine,147(03):363-379.
Melluso, L., Mahoney, J.J. and Dallai, L.,2006. Mantle sources and crustal input as recorded in high-Mg Deccan Traps basalts of Gujarat (India). Lithos,89(3-4):259-274.
Marsh, B.D.,1981. On the crystallinity, probability of occurrence, and rheology of lava and magma. Contributions to Mineralogy and Petrology,78(1):85-98.
Marsh, B.D.,1988. Crystal size distribution (CSD) in rocks and the kinetics and dynamics of crystallization. Contributions to Mineralogy and Petrology,99(3):277-291.
Marsh, B.D.,1996. Solidification fronts and magmatic evolution. Mineralogical Magazine,60(1):5-40.
Marsh, B.D.,1998. On the Interpretation of Crystal Size Distributions in Magmatic Systems. Journal of Petrology,39(4):553-599.
Martin, V.M., Davidson, J., Morgan, D. and Jerram, D.A.,2010. Using the Sr isotope compositions of feldspars and glass to distinguish magma system components and dynamics. Geology,38(6):539-542.
Melnik, O. and Sparks, R.S.I.,2002. Dynamics of magma ascent and lava extrusion at Soufriere Hills Volcano, Montserrat. Geological Society,21:153-171
Miller, J.S. and Wooden, J.L.,2004. Residence,resorption and recycling of zicons in Devils Kitchen Rhyolite,Coso Volcanic Field,California. J. Petrology,45(11):2155-2170
Mills, R.D., Ratner, J.J. and Glazner, A.F.,2011. Experimental evidence for crystal coarsening and fabric development during temperature cycling. Geology,39(12):1139-1142.
Mock, A. and Jerram, D.A.,2005. Crystal Size Distributions (CSD) in Three Dimensions:Insights from the3D Reconstruction of a Highly Porphyritic Rhyolite. Journal of Petrology,46(8):1525-1541.
Molloy, C, Shane, Phil, and Nairn, Ⅰ,2008. Pre-eruption thermal rejuvenation and stirring of a partly crystalline rhyolite pluton revealed by the Earthquake Flat Pyroclastics deposit, New Zealand. Journal of the Geological Society,165:435-447
Morgan, D.J. and Jerram, D.A.,2006. On estimating crystal shape for crystal size distribution analysis. Journal of Volcanology and Geothermal Research,154(1-2):1-7.
Morgan, D.J., Jerram, D.A., Chertkoff, D.G., Davidson, J.P., Pearson, D.G., Kronz, A. and Nowell, G.M.,2007. Combining CSD and isotopic microanalysis:Magma supply and mixing processes at Stromboli Volcano, Aeolian Islands, Italy. Earth and Planetary Science Letters,260(3-4):419-431.
Morgan, W.J.,1971. Convection Plumes in the Lower Mantle. Nature,230(5288):42-43.
Pang, K.-N., Li, C, Zhou, M.-F. and Ripley, E.,2008a. Abundant Fe-Ti oxide inclusions in olivine from the Panzhihua and Hongge layered intrusions, SW China:evidence for early saturation of Fe-Ti oxides in ferrobasaltic magma. Contributions to Mineralogy and Petrology,156(3):307-321.
Pang, K.N., Li, C, Zhou, M.F. and Ripley, E.M.,2009. Mineral compositional constraints on petrogenesis and oxide ore genesis of the late Permian Panzhihua layered gabbroic intrusion, SW China. Lithos,110(1-4):199-214.
Pang, K.N., Zhou, M.F., Lindsley, D., Zhao, D. and Malpas, J.,2008b. Origin of Fe-Ti Oxide Ores in Mafic Intrusions:Evidence from the Panzhihua Intrusion, SW China. Journal of Petrology,49(2):295-313.
Parsons, I.,1987. Origins of igneous layering. Springer.
Patwardhan, K. and Marsh, B.D.,2011. Dynamics of the Development of the Isle au Haut Gabbro-Diorite Layered Complex:Quantitative Implications for Mafic-Silicic Magma Interactions. Journal of Petrology,52(12):2365-2395.
Pearce, J. and Norry, M.,1979. Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks. Contributions to Mineralogy and Petrology,69(1):33-47.
Peate, D.W, Hawkesworth, C.J., Mantovani, M.M., Rogers, N.W and Turner, S.P.,1999. Petrogenesis and stratigraphy of the high-Ti/Y Urubici magma type in the Parana flood basalt province and implications for the nature of'Dupal'-type mantle in the South Atlantic region. Journal of Petrology,40(3):451-473.
Pik, R., Deniel, C, Coulon, C, Yirgu, G., Hofmann, C. and Ayalew, D.,1998. The northwestern Ethiopian Plateau flood basalts:classification and spatial distribution of magma types. Journal of Volcanology and Geothermal Research,81(1):91-111.
Putirka, K.D.,2005. Igneous thermometers and barometers based on plagioclase＋liquid equilibria:Tests of some existing models and new calibrations. American Mineralogist,90(2-3):336-346.
Putirka, K.D.,2008. Thermometers and Barometers for Volcanic Systems. Reviews in Mineralogy and Geochemistry,69(1):61-120.
Ramos, F.C., Wolff, J.A. and Tollstrup, D.L.,2004. Measuring87Sr/86Sr variations in minerals and groundmass from basalts using LA-MC-ICPMS. Chemical Geology,211(1-2):135-158.
Revillon, S., Arndt, N., Hallot, E., Kerr, A. and Tarney, J.,1999. Petrogenesis of picrites from the Caribbean Plateau and the North Atlantic magmatic province. Lithos,49(1):1-21.
Salisbury, M.J., Bohrson, W.A., Clynne, M.A., Ramos, E.C. and Hoskin, P.,2008. Multiple Plagioclase Crystal Populations Identified by Crystal Size Distribution and in situ Chemical Data:Implications for Timescales of Magma Chamber Processes Associated with the1915Eruption of Lassen Peak, CA. Journal of Petrology,49(10):1755-1780.
Scarfe, C.M., Cronin, D.J., Wenzel, J.T. and Kauffman, D.A.,1983. Viscosity-temperature relationships at1atm in the system diopside-anorthite. Amer. Mineral.68,1083-1088
Sen, G.,2001. Generation of Deccan Trap magmas. J Earth Syst Sci,110(4):409-431.
Shane, P., Martin, S.B., Smith, V.C., Beggs, K.F., Darragh, M.B., Cole, J.W. and Nairn,I.A.2007. Multiple rhyolite magmas and basalt injection in the17.7ka Rerewhakaaitu eruption episode from Tarawera volcanic complex, New Zealand. Journal of Volcanology and Geothermal Research,164:1-26
Shaw, H.R.,1972.Viscosities of magmatic silicate liquids:An empirical method of prediction,Am.J. Sci,272:870-893
Shellnutt, J.G. and Jahn, B.M.,2010. Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex:Implications for the genesis of Fe-Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters,289(3-4):509-519.
Shellnutt, J.G, Wang, K.L., Zellmer, G.F., Iizuka, Y., Jahn, B.M., Pang, K.N., Qi, L. and Zhou, M.F.,2011. Three Fe-Ti oxide ore-bearing gabbro-granitoid complexes in the Panxi region of the Permian Emeishan large igneous province, SW China. American Journal of Science,311(9):773-812.
Shellnutt, J., Zhou, M.F., Yan, D.P. and Wang, Y.B.,2008. Longevity of the Permian Emeishan mantle plume (SW China):1Ma,8Ma or18Ma? Geological Magazine,145(3):373-388.
Shellnutt, J.G., Zhou, M.F. and Zellmer, G.F.,2009. The role of Fe-Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap:An example from the Permian Baima igneous complex, SW China. Chemical Geology,259(3-4):204-217.
Shellnutt, J.G., Denyszyn, S.W. and Mundil, R.,2012. Precise age determination of mafic and felsic intrusive rocks from the Permian Emeishan large igneous province (SW China). Gondwana Research,22(1):118-126.
Simakin, A.G. and Bindeman, I.N.,2008. Evolution of crystal sizes in the series of dissolution and precipitation events in open magma systems. Journal of Volcanology and Geothermal Research,177(4):997-1010.
Sobolev, A.V., Hofmann, A.W., Kuzmin, D.V., Yaxley, G.M., Arndt, N.T., Chung, S.-L. Danyushevsky, L.V., Elliott, T., Frey, F.A., Garcia, M.O., Gurenko, A.A., Kamenetsky, V.S., Kerr, A.C., Krivolutskaya, N.A., Matvienkov, V.V., Nikogosian, I.K., Rocholl, A., Sigurdsson, I.A., Sushchevskaya, N.M. and Teklay, M.,2007. The Amount of Recycled Crust in Sources of Mantle-Derived Melts. Science,316(5823):412-417.
Solano, J.M.S., Jackson, M.D., Sparks, R.S.J., Blundy, J.D. and Annen, C.,2012. Melt Segregation in Deep Crustal Hot Zones:a Mechanism for Chemical Differentiation, Crustal Assimilation and the Formation of Evolved Magmas. Journal of Petrology,53(10):1999-2026.
Song, X.Y., Zhou, M.F., Cao, Z.M., Sun, M. and Wang, Y.L.,2003. Ni-Cu-(PGE) magmatic sulfide deposits in the Yangliuping area, Permian Emeishan igneous province, SW China. Miner Deposita,38(7):831-843.
Song, X.Y, Zhou, M.F., Hou, Z.Q., Cao, Z.-M., Wang, Y.-L. and Li, Y.,2001. Geochemical Constraints on the Mantle Source of the Upper Permian Emeishan Continental Flood Basalts, Southwestern China. International Geology Review,43(3):213-225.
Sun, S.S. and McDonough, W.F.,1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. Geological Society, London, Special Publications,42(1):313-345.
Suzuki, Y. and Nakada, S.,2007. Remobilization of highly crystalline felsic magma by injection of mafic magma:Constraints from the middle sixth century eruption at Haruna volcano, Honshu, Japan. Journal of Petrology,48(8):1543-1567.
Tao, Y., Li, C, Song, X.Y. and Ripley, E.,2008. Mineralogical, petrological, and geochemical studies of the Limahe mafic-ultramatic intrusion and associated Ni-Cu sulfide ores, SW China. Miner Deposita,43(8):849-872.
Taylor, S.R. and McLennan, S.M.,1985. The continental crust:Its composition and evolution, Medium:X; Size:Pages:328pp.
Ukstins-Peate, I. and Bryan, S.E.,2008. Re-evaluating plume-induced uplift in the Emeishan large igneous province. Nature Geosci,1(9):625-629.
Vance, J.,1969. On synneusis. Contributions to Mineralogy and Petrology,24(1):7-29.
Vinet, N. and Higgins, M.D.,2010. Magma Solidification Processes beneath Kilauea Volcano, Hawaii:a Quantitative Textural and Geochemical Study of the1969-1974Mauna Ulu Lavas. Journal of Petrology,51(6):1297-1332.
Wager, L. and Brown, G,1967. Layered Igneous Rocks,588. Oliver and Boyd, San Francisco.
Wagner, C.,1961. Theorie der Alterung von Niederschlagen durch Umlosen (Ostwald-Reifung). Zeitschrift fur Elektrochemie, Berichte der Bunsengesellschaft fur physikalische Chemie,65(7-8):581-591.
Wang, C, Zhou, M.F. and Keays, R.,2006. Geochemical constraints on the origin of the Permian Baimazhai mafic-ultramafic intrusion, SW China. Contributions to Mineralogy and Petrology,152(3):309-321.
Wang, C.Y., Zhou, M.F. and Qi, L.,2007. Permian flood basalts and mafic intrusions in the Jinping (SW China)-Song Da (northern Vietnam) district:Mantle sources, crustal contamination and sulfide segregation. Chemical Geology,243(3-4):317-343.
Wang, C, Zhou, M.F., Sun, Y. and Arndt, N.,2012. Differentiation, crustal contamination and emplacement of magmas in the formation of the Nantianwan mafic intrusion of the-260Ma Emeishan large igneous province, SW China. Contributions to Mineralogy and Petrology,164(2):281-301.
Wang, C.Y., Zhou, M.F. and Zhao, D.,2005. Mineral chemistry of chromite from the Permian Jinbaoshan Pt-Pd-sulphide-bearing ultramafic intrusion in SW China with petrogenetic implications. Lithos,83(1):47-66.
Wang, K., Plank, T., Walker, J.D., et al.,2002. A mantle melting profile across the Basin and Range,SWUSA. Journal of Geophysical Research,107(B1),doi:10.1029/2001JB000209
Wang, Y., Zhang, X.M., Jiang, C.S., Wei, H.Q. and Wan, J.L.,2007. Tectonic controls on the late Miocene-Holocene volcanic eruptions of the Tengchong volcanic field along the southeastern margin of the Tibetan plateau. Journal of Asian Earth Sciences,30:375-389
Wiebe, R.A., Manon, M.R., Hawkins, D.P. and McDonough, W.F.,2004. Late-stage mafic injection and thermal rejuvenation of the Vinalhaven granite, Coastal Maine. Journal of Petrology,45(11):2133-2153
Williams, E., Boudreau, A.E., Boorman, S. and Kruger, F.J.,2006. Textures of orthopyroxenites from the Burgersfort bulge of the eastern Bushveld Complex, Republic of South Africa. Contributions to Mineralogy and Petrology,151(4):480-492.
Wilson, J.T.,1963. A POSSIBLE ORIGIN OF THE HAWAIIAN ISLANDS. Canadian Journal of Physics,41(6):863-870.
Xiao, L., Xu, Y.G., Mei, H.J., Zheng, Y.F., He, B. and Pirajno, F.,2004. Distinct mantle sources of low-Ti and high-Ti basalts from the western Emeishan large igneous province, SW China: implications for plume-lithosphere interaction. Earth and Planetary Science Letters,228(3-4):525-546.
Xu, Y.G., Chung, S.L., Shao, H. and He, B.,2010. Silicic magmas from the Emeishan large igneous province, Southwest China:Petrogenesis and their link with the end-Guadalupian biological crisis. Lithos,119(1-2):47-60.
Xu, Y.G., He, B., Chung, S.L., Menzies, M.A. and Frey, F.A.,2004. Geologic, geochemical, and geophysical consequences of plume involvement in the Emeishan flood-basalt province. Geology,32(10):917-920.
Xu, Y.G., Luo, Z.Y., Huang, X.L., He, B., Xiao, L., Xie, L.W and Shi, Y.R.,2008. Zircon U-Pb and Hf isotope constraints on crustal melting associated with the Emeishan mantle plume. Geochimicaet Cosmochimica Acta,72(13):3084-3104.
Xu, Y.G., Chung, S.L., Jahn, B.M. and Wu, G.,2001. Petrologic and geochemical constraints on the petrogenesis of Permian-Triassic Emeishan flood basalts in southwestern China. Lithos,58(3-4):145-168.
Yang, Z.F.,2012. Combining Quantitative Textural and Geochemical Studies to Understand the Solidification Processes of a Granite Porphyry:Shanggusi, East Qinling, China. Journal of Petrology,53(9):1807-1835.
Zellmer, G.F., Blake, S., Vance, D., Hawkesworth, C. and Turner, S.,1999. Plagioclase residence times at two island arc volcanoes (Kameni Islands, Santorini, and Soufriere, St. Vincent) determined by Sr diffusion systematics. Contributions to Mineralogy and Petrology,136(4):345-357.
Zellmer, G.F., Sparks, R.S.J., Hawkesworth, C.J. and Wiedenbeck, M.,2003. Magma Emplacement and Remobilization Timescales Beneath Montserrat:Insights from Sr and Ba Zonation in Plagioclase Phenocrysts. J. Petrology,44(8):1413-1431
Zhang, Z., Mahoney, J.J., Mao, J. and Wang, F.,2006. Geochemistry of Picritic and Associated Basalt Flows of the Western Emeishan Flood Basalt Province, China. Journal of Petrology,47(10):1997-2019.
Zhang, Z., Mao, J., Saunders, A.D., Ai, Y., Li, Y. and Zhao, L.,2009. Petrogenetic modeling of three mafic-ultramafic layered intrusions in the Emeishan large igneous province, SW China, based on isotopic and bulk chemical constraints. Lithos,113(3-4):369-392.
Zhang, Z., Zhi, X., Chen, L., Saunders, A.D. and Reichow, M.K.,2008. Re-Os isotopic compositions of picrites from the Emeishan flood basalt province, China. Earth and Planetary Science Letters,276(1-2):30-39.
Zhong, H., Qi, L., Hu, R.Z., Zhou, M.F., Gou, T.Z., Zhu, W.G., Liu, B.G. and Chu, Z.Y.,2011. Rhenium-osmium isotope and platinum-group elements in the Xinjie layered intrusion, SW China:Implications for source mantle composition, mantle evolution, PGE fractionation and mineralization. Geochimica et Cosmochimica Acta,75(6):1621-1641.
Zhong, H., Yao, Y, Prevec, S.A., Wilson, A.H., Viljoen, M.J., Viljoen, R.P., Liu, B.-G. and Luo, Y.-N.,2004. Trace-element and Sr-Nd isotopic geochemistry of the PGE-bearing Xinjie layered intrusion in SW China. Chemical Geology,203(3-4):237-252.
Zhong, H., Zhu, W.G., Hu, R.Z., Xie, L.W, He, D.F., Liu, F. and Chu, Z.Y.,2009. Zircon U-Pb age and Sr-Nd-Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos,110(1-4):109-128.
Zhong, Y.T., He, B,, Mundil, R., Xu, Y.G.2014. CA-TIMS zircon U-Pb dating of felsic ignimbrite from the Binchuan section:Implications for the termination age of Emeishan large igneous province. Lithos,10.1016/j.lithos.2014.03.005
Zhou, M.F., Arndt, N.T., Malpas, J., Wang, C.Y. and Kennedy, A.K.,2008. Two magma series and associated ore deposit types in the Permian Emeishan large igneous province, SW China. Lithos,103(3):352-368.
Zhou, M.F., Chen, W.T., Wang, C.Y., Prevec, S.A., Liu, Patricia P. and Howarth, G.H.,2013. Two stages of immiscible liquid separation in the formation of Panzhihua-type Fe-Ti-V oxide deposits, SW China. Geoscience Frontiers,4(5):481-502.
Zhou, M.F., Malpas, J., Song, X.Y., Robinson, P.T., Sun, M., Kennedy, A.K., Lesher, C.M. and Keays, R.R.,2002. A temporal link between the Emeishan large igneous province (SW China) and the end-Guadalupian mass extinction. Earth and Planetary Science Letters,196(3-4):113-122.
Zhou, M.F., Robinson, P.T., Lesher, C.M., Keays, R.R., Zhang, C.-J. and Malpas, J.,2005. Geochemistry, Petrogenesis and Metallogenesis of the Panzhihua Gabbroic Layered Intrusion and Associated Fe-Ti-V Oxide Deposits, Sichuan Province, SW China. Journal of Petrology,46(11):2253-2280.
Zhu, B., Guo, Z., Liu, R., Liu, D. and Du, W.,2014. No pre-eruptive uplift in the Emeishan large igneous province:New evidences from its'inner zone', Dali area, Southwest China. Journal of Volcanology and Geothermal Research,269(0):57-67.
Zhu, B.Q., Mao, C.X., Lugmair, G.W. and Macdougall, J.D.,1983. Isotopic and geochemical evidence for the origin of Plio-Pleistocene volcanic rocks near the Indo2Eurasian collisional margin at Tengchong, China[J]. Earth Planet. Sci. Lett.65(2):263-275.
Zieg, M.J. and Marsh, B.D.,2002. Crystal Size Distributions and Scaling Laws in the Quantification of Igneous Textures. Journal of Petrology,43(1):85-101.
何斌,徐义刚,肖龙等.2006.峨眉山地幔柱上升的沉积相应及其地质意义.地质论评,52(1)：30-37
侯增谦,卢记仁,汪云亮,夏林圻,李红阳和国连杰,1999.峨眉火成岩省：结构、成因与特色.地质论评(S1)：885-891.
皇甫岗,石绍先,苏有锦.2000.20世纪云南地震活动研究.地震研究,23(1)：1-9
季建清.1998.腾冲地块西缘岛弧地体中发现洋壳残片.地学前缘,5(3)：50-55
季建清.2000.滇西南新生代走滑断裂运动学、年代学、及对青藏高原东南部块体运动的意义.地质科学,35(3)：336-349
李宏博,张招崇和吕林素,2010.峨眉山大火成岩省基性墙群几何学研究及对地幔柱中心的指示意义.岩石学报(10)：3143-3152.
李廷栋.2010.中国岩石圈的基本特征.地学前缘,17(3)：2-13
李佑国.2007.基于“3S”技术的攀西地区铜镍铂族元素矿床找靶筛选[C].成都：成都理工大学
梁涛,罗照华,李德东等.2008.托云盆地新生代幔源岩浆源区起止深度的限定.岩石学报,024(11)：2820-2838
梁涛,罗照华,李文韬等.2005.托云火山群的火山地质特征及其构造意义.新疆地质,23(2)：105-110
刘杕,沈发奎,张光宗.攀西地区层状岩体[A].张云湘主编.中国攀西裂谷文集[C].北京：地质出版社,1985：85-118
罗照华,辛后田,陈必河,柯珊和黄金香.2007.壳幔过渡层及其大陆动力学意义.现代地质,21(2)：421-425
罗照华,莫宣学,侯增谦等.2006.青藏高原新生代形成演化的整合模型——来自火成岩的约束.地学前缘,13(4)：196-211
罗照华,卢欣祥,郭少丰,孙静,陈必河,黄凡和杨宗锋.2008a.透岩浆流体成矿体系.岩石学报(12)：2669-2678.
罗照华,卢欣祥,刘翠,李德东,杨宗锋和文思博.2011.岩浆热液成矿理论的失败：原因和出路.吉林大学学报(地球科学版)(01)：1-11.
罗照华,卢欣祥,王秉璋,陈必河,黄凡,杨宗锋和汪洋.2008b.造山后脉岩组合与内生成矿作用.地学前缘(04)：1-12.
罗照华,刘嘉麒,赵慈平,郭正府,程黎鹿,李晓惠,李大鹏.2010a.深部流体与岩浆活动：兼论腾冲火山群的深部过程。岩石学报,027(10)：2855-62
罗照华,卢欣祥,许俊玉,刘翠,李德东.2010b.成矿侵入体的岩石学标志.岩石学报,026(8)：2247-54
罗照华,莫宣学,卢欣祥,陈必河,柯珊,侯增谦和江万.2007.透岩浆流体成矿作用——理论分析与野外证据.地学前缘(03)：165-183
邱家骧.1991.应用岩浆岩岩石学.中国地质大学出版社.155-158
史仁灯,郝艳丽和黄启帅,2008.Re-Os同位素对峨眉山大火成岩省成因制约的探讨.岩石学报(11)：2515-2523.
宋谢炎,张成江,胡瑞忠等.2005.峨眉火成岩省岩浆矿床成矿作用与地幔柱动力学过程的耦合关系.矿物岩石,25(4)：35-44
汤庆艳,张铭杰,余明,王启立,尚慧,2013.晚二叠世峨眉山地幔柱岩浆成矿作用.岩石矿物学杂志,32(5)：680-692
佟伟,章铭陶.1989.腾冲地热[M].北京：科学出版社.
向才英,周真恒,姜朝松.2000.腾冲火山岩岩石化学研究.云南地质,19(2)：134-151
徐义刚,何斌,黄小龙,罗震宇,朱丹,马金龙和邵辉,2007.地幔柱大辩论及如何验证地幔柱假说.地学前缘(02)：1-9.
云南省地质局.1982.腾冲幅和盈江幅(1：200000)区域地质调查报告.
云南省地质矿产局.1985腾冲幅和朗蒲寨幅(1：50000)区域地质调查报告..
云南省地质矿产局.1992.古永幅(1：50000)区域地质调查报告.
张辉煌,徐义刚,葛文春,等.2006.吉林伊通—大屯地区晚中生代—新生代玄武岩的地球化学特征及其意义.岩石学报,22(6)：1579-1596
赵慈平.2008.腾冲火山区现代幔源氦释放特征及深部岩浆活动你个岩浆.学位论文.
赵志丹,莫宣学,罗照华等.2003.印度—亚洲俯冲带结构—岩浆作用证据.地学前缘,10(3)：149-157
钟宏,徐桂瘟,朱维光等.2009.峨眉山大火成岩省太和花岗岩的成因及构造意义.矿物岩石地球化学通报,28(2)：99-110
周真恒,韩新民,周瑞琦.1996.云南腾冲地区的岩石圈热结构.地震地磁观测与研究,17(4)：34-41
Ali, J.R., Lo, C.H., Thompson, G.M. and Song, X.,2004. Emeishan Basalt Ar-Ar overprint ages define several tectonic events that affected the western Yangtze platform in the Mesozoic and Cenozoic. Journal of Asian Earth Sciences,23(2):163-178.
Ali, J.R., Thompson, G.M., Zhou, M.F. and Song, X.,2005. Emeishan large igneous province, SW China. Lithos,79(3-4):475-489.
Anderson, D.L.,2005. Large Igneous Provinces, Delamination, and Fertile Mantle. Elements,1(5):271-275.
Annen, C, Blundy, J.D. and Sparks, R.S.J.,2006. The Genesis of Intermediate and Silicic Magmas in Deep Crustal Hot Zones. Journal of Petrology,47(3):505-539.
Armienti, P., Perinelli, C. and Putirka, K.D.,2012. A New Model to Estimate Deep-level Magma Ascent Rates, with Applications to Mt. Etna (Sicily, Italy). Journal of Petrology.
Arndt, N., Chauvel, C, Czamanske, G. and Fedorenko, V.,1998. Two mantle sources, two plumbing systems:tholeiitic and alkaline magmatism of the Maymecha River basin, Siberian flood volcanic province. Contributions to Mineralogy and Petrology,133(3):297-313.
Bachmann, O. and Bergantz, G.W.,2003. Rejuvenation of the Fish Canyonmagma body:a window into the evolution of large-volume silicic magma systems. Geology,31:789-792.
Bachmann, O. and Bergantz, G.,2006. Gaspercolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies, Journal of Volcanology and Geothermal research,149:85-102
Bachmann, O., Michael, A.D. and Peter, W.L.,2002. The fish canyon magma body,san juan volcanic field, colorado:rejuvenation and eruption of an upper-crustal batholith. Journal of petrology.23:1469-1503
Beane, J.E., Turner, C.A., Hooper, P.R., Subbarao, K.V. and Walsh, J.N.,1986. Stratigraphy, composition and form of the Deccan Basalts, Western Ghats, India. Bulletin of Volcanology,48(1):61-83.
Blundy, J. and Cashman, K.,2001. Ascent-driven crystallisation of dacite magmas at Mount St Helens,1980-1986. Contrib Mineral Petrol,140:631-650
Boorman, S., Boudreau, A. and Kruger, F.J.,2004. The Lower Zone-Critical Zone Transition of the Bushveld Complex:a Quantitative Textural Study. Journal of Petrology,45(6):1209-1235.
Bryan, S.E. and Ernst, R.E.,2008. Revised definition of Large Igneous Provinces (LIPs). Earth-Science Reviews,86(1-4):175-202.
Bryan, S.E., Peate, I.U., Peate, D.W., Self, S., Jerram, D.A., Mawby, M.R., Marsh, J.S. and Miller, J.A.,2010. The largest volcanic eruptions on Earth. Earth-Science Reviews,102(3-4):207-229.
Burgisser, A. and Bergantz, G.W.,2011. A rapid mechanism to remobilize and homogenize highly crystalline magma bodies. Nature,471:212-215
Campbell, I,H, and Turnerm J.S.,1985. Turbulent mixing between fluids with different viscosities.Nature,313:39-42
Campbell, I.H. and Turner, J.S.,1986. The influence of viscosity on fountains in magma chambers. J.Petrology,27:1-30
Cashman, K.V.,1993. Relationship between plagioclase crystallization and cooling rate in basaltic melts. Contributions to Mineralogy and Petrology,113(1):126-142.
Cashman, K.V. and Marsh, B.D.,1988. Crystal size distribution (CSD) in rocks and the kinetics and dynamics of crystallization II:Makaopuhi lava lake. Contributions to Mineralogy and Petrology,99(3):292-305.
Chandrasekharam, D., Mahoney, J.J., Sheth, H.C. and Duncan, R.A.,1999. Elemental and Nd-Sr-Pb isotope geochemistry of flows and dikes from the Tapi rift, Deccan flood basalt province, India. Journal of Volcanology and Geothermal Research,93(1-2):111-123.
Cheikh, N.D., Beya, B.B. and Lili, T.2007. Natural convection flow in a tall enclosure using a multigrid method. C.R.Mecanique.335,113-118
Cheng, L.L., Yang, Z.F., Zeng, L., Wang, Y. and Luo, Z.H.,2014. Giant plagioclase growth during storage of basaltic magma in Emeishan Large Igneous Province, SW China. Contributions to Mineralogy and Petrology,167(2):1-20.
Chung, S.L. and Jahn, B.M.,1995. Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary. Geology,23(10):889-892.
Chung, S.L., Jahn, B., Genyao, W., Lo, C.H. and Bolin, C.,1998. The Emeishan flood basalt in SW China:A mantle plume initiation model and its connection with continental breakup and mass extinction at the Permian-Triassic Boundary, Mantle Dynamics and Plate Interactions in East Asia. Geodyn. Ser. AGU, Washington, DC, pp.47-58.
Coffin, M.F. and Eldholm,O.,1994. Large igneous provinces:crustal structure, dimensions, and external consequences. Reviews of Geophysics,32(1):1-36.
Couch, S., Sparks, R.S.J. and Carroll, M.R.,2001. Mineral disequilibrium in lavas explained by convective self-mixing in open magma chambers. Nature,411:1037-1039
Couch, S., Sparks, R.S.J. and Carroll, M.R.,2003. The Kinetics of Degassing-Induced Crystallization at Soufriere Hills Volcano, Montserrat. Journal of Petrology,44(8):1477-1502.
Cordier, C, Caroff, M. and Rannou, E.,2012. Timescale of open-reservoir evolution beneath the south Cleft segment, Juan de Fuca ridge. Mineralogy and Petrology,104(1-2):1-14.
Cox, K.G.,1980. A Model for Flood Basalt Vulcanism. Journal of Petrology,21(4):629-650.
Cox, K.G.M., R.; Hornung G.,1967. Geochemical and petrographic provinces in the Karoo basalts of southern Africa. American Mineralogist,52:1451-1474.
DeHoff, R.T.,1991. A geometrically general theory of diffusion controlled coarsening. Acta Metallurgica et Materialia,39(10):2349-2360.
Dong, H., Xing, C. and Wang, C.Y.,2013. Textures and mineral compositions of the Xinjie layered intrusion, SW China:Implications for the origin of magnetite and fractionation process of Fe-Ti-rich basaltic magmas. Geoscience Frontiers,4(5):503-515.
Elburg, M., Vroon, P., van der Wagt, B. and Tchalikian, A.,2005. Sr and Pb isotopic composition of five USGS glasses (BHVO-2G, BIR-1G, BCR-2G, TB-1G, NKT-1G). Chemical Geology,223(4):196-207.
Ernst, R.E., Buchan, K.L. and Campbell, I.H.,2005. Frontiers in large igneous province research. Lithos,79(3-4):271-297.
Ewart, A., Marsh, J.S., Milner, S.C., Duncan, A.R., Kamber, B.S. and Armstrong, R.A.,2004. Petrology and Geochemistry of Early Cretaceous Bimodal Continental Flood Volcanism of the NW Etendeka, Namibia. Part1:Introduction, Mafic Lavas and Re-evaluation of Mantle Source Components. Journal of Petrology,45(1):59-105.
Ewart, A., Milner, S.C., Armstrong, R.A. and Dungan, A.R.,1998. Etendeka Volcanism of the Goboboseb Mountains and Messum Igneous Complex, Namibia. Part I:Geochemical Evidence of Early Cretaceous Tristan Plume Melts and the Role of Crustal Contamination in the Parana-Etendeka CFB. Journal of Petrology,39(2):191-225.
Fan, W., Zhang, C, Wang, Y., Guo, F. and Peng, T.,2008. Geochronology and geochemistry of Permian basalts in western Guangxi Province, Southwest China:Evidence for plume-lithosphere interaction. Lithos,102(1-2):218-236.
Freysteinn et al (2010) Freysteinn S et al.2010. Intrusion triggering of the2010Eyjafjallajokull explosive eruption. Nature.468:426-430
Ganino, C, Arndt, N., Zhou, M.-F, Gaillard, F. and Chauvel, C.,2008. Interaction of magma with sedimentary wall rock and magnetite ore genesis in the Panzhihua mafic intrusion, SW China. Miner Deposita,43(6):677-694.
Ghiorso, M. and Sack, R.,1995. Chemical mass transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures. Contributions to Mineralogy and Petrology,119(2-3):197-212.
Griffiths, R.W. and Campbell, I.H.,1990. Stirring and structure in mantle starting plumes. Earth and Planetary Science Letters,99(1):66-78.
Hanski, E., Kamenetsky, V.S., Luo, Z.-Y., Xu, Y.-G. and Kuzmin, D.V.,2010. Primitive magmas in the Emeishan Large Igneous Province, southwestern China and northern Vietnam. Lithos,119(1-2):75-90.
He, B., Xu, Y. and Campbell, I.,2009. Pre-eruptive uplift in the Emeishan? Nature Geosci,2(8):530-531.
He, B., Xu, Y.G., Chung, S.L., Xiao, L. and Wang, Y.,2003. Sedimentary evidence for a rapid, kilometer-scale crustal doming prior to the eruption of the Emeishan flood basalts. Earth and Planetary Science Letters,213(3-4):391-405.
He, B., Xu, Y.G., Huang, X.L., Luo, Z.Y., Shi, Y.R., Yang, Q.J. and Yu, S.Y.,2007. Age and duration of the Emeishan flood volcanism, SW China:Geochemistry and SHRIMP zircon U-Pb dating of silicic ignimbrites, post-volcanic Xuanwei Formation and clay tuff at the Chaotian section. Earth and Planetary Science Letters,255(3-4):306-323.
Higgins, M.D.,1994. Determination of crystal morphology and size from bulk measurements on thin sections:numerical modelling. American Mineralogist,79:113-119.
Higgins, M.D.,1996. Magma dynamics beneath Kameni volcano, Thera, Greece, as revealed by crystal size and shape measurements. Journal of Volcanology and Geothermal Research,70(1-2):37-48.
Higgins, M.D.,1998. Origin of Anorthosite by Textural Coarsening:Quantitative Measurements of a Natural Sequence of Textural Development. Journal of Petrology,39(7):1307-1323.
Higgins, M.D.,2000. Measurement of crystal size distributions. American Mineralogist,85(9):1105-1116.
Higgins, M.D.,2006. Verification of ideal semi-logarithmic, lognormal or fractal crystal size distributions from2D datasets. Journal of Volcanology and Geothermal Research,154:8-16.
Higgins, M.D.,2009. The Cascadia megathrust earthquake of1700may have rejuvenated an isolated basalt volcano in western Canada:Age and petrographic evidence. Journal of Volcanology and Geothermal Research,179(1-2):149-156.
Higgins, M.D.,2011a. Quantitative petrological evidence for the origin of K-feldspar megacrysts in dacites from Taapaca volcano, Chile. Contributions to Mineralogy and Petrology,162(4):709-723.
Higgins, M.D.,2011b. Textural coarsening in igneous rocks. International Geology Review,53(3-4):354-376.Higgins, M.D. and Chandrasekharam, D.,2007. Nature of Sub-volcanic Magma Chambers, Deccan Province, India:Evidence from Quantitative Textural Analysis of Plagioclase Megacrysts in the Giant Plagioclase Basalts. Journal of Petrology,48(5):885-900.
Hildreth W.2007. Quaternary Magmatism in the Cascades:Geo-logical Perspectives[M]. USGS Professional Paper,1744:1-125.
Hooper, P.R.,1997. The Columbia River flood basalt province:Current status, Large Igneous Provinces:Continental, Oceanic, and Planetary Flood Volcanism. Geophys. Monogr. Ser. AGU, Washington, DC, pp.1-27.
Hooper, P.R., Subbarao, K.V. and Beane, J.E.,1988. The giant plagioclase basalts (GPBs) of the western Ghats, Deccan Traps. Geological Society of India Memoir,10:135-144.
Hossain, M.A. and Wilson,M.2002. Natural convection flow in a fluid-saturated porous medium enclosed by non-isothermal walls with heat generation.Int. J.Therm.Sci.41,447-454
Hou, T., Zhang, Z., Encarnacion, J., Santosh, M. and Sun, Y.,2013. The role of recycled oceanic crust in magmatism and metallogeny:Os-Sr-Nd isotopes, U-Pb geochronology and geochemistry of picritic dykes in the Panzhihua giant Fe-Ti oxide deposit, central Emeishan large igneous province, SW China. Contributions to Mineralogy and Petrology,165(4):805-822.
Hou, T., Zhang, Z., Kusky, T., Du, Y., Liu, J. and Zhao, Z.,2011. A reappraisal of the high-Ti and low-Ti classification of basalts and petrogenetic linkage between basalts and mafic-ultramafic intrusions in the Emeishan Large Igneous Province, SW China. Ore Geology Reviews,41(1):133-143.
Howarth, G.H. and Prevec, S.A.,2013. Hydration vs. oxidation:Modelling implications for Fe-Ti oxide crystallisation in mafic intrusions, with specific reference to the Panzhihua intrusion, SW China. Geoscience Frontiers,4(5):555-569.
Huber, C, Bachmann, O. and Dufek, J.,2010. The limitations of melting on the reactivation of silicic mushes. J. Volcanol. Geotherm. Res.,195:97-105
Hummel, W. and Arndt, J.,1985. Variation of viscosity with temperature and composition in the plagioclase system. Contrib Mineral Petrol,90:83-92
Huppert, H.E. and Sparks, R.S.J.,1988. The generation of granitic magmas by intrusion of basalt into continental crust. J. Petrol,29:599-624
Irvine, T.N.,1975. Crystallization sequences in the Muskox intrusion and other layered intrusions—Ⅱ. Origin of chromitite layers and similar deposits of other magmatic ores. Geochimica et Cosmochimica Acta,39(6-7):991-1020.
Jerram, D.A. and Martin, V.M.,2008. Understanding crystal populations and their significance through the magma plumbing system. Geological Society, London, Special Publications,304(1):133-148.
Kamenetsky, V.S., Chung, S.L., Kamenetsky, M.B. and Kuzmin, D.V.,2012. Picrites from the Emeishan Large Igneous Province, SW China:a Compositional Continuum in Primitive Magmas and their Respective Mantle Sources. Journal of Petrology,53(10):2095-2113.
Lange, R.A., Frey, H.M. and Hector, J.,2009. A thermodynamic model for the plagioclase-liquid hygrometer/thermometer. American Mineralogist,94(4):494-506.
Langmuir, C.H., Klein, E.M. and Plank, T.,1992. Petrological systematics of mid-ocean ridge basalts:Constraints on melt generation beneath ocean ridges. Geophysical Monograph Series,71:183-280.
Lai, S., Qin, J., Li, Y., Li, S. and Santosh, M.,2012. Permian high Ti/Y basalts from the eastern part of the Emeishan Large Igneous Province, southwestern China:Petrogenesis and tectonic implications. Journal of Asian Earth Sciences,47(0):216-230.
Larsen, L.M. and Pedersen, A.K.,2000. Processes in high-Mg, high-T magmas:evidence from olivine, chromite and glass in Palaeogene picrites from West Greenland. Journal of Petrology,41(7):1071-1098.
Li, C, Tao, Y., Qi, L. and Ripley, E.M.,2012. Controls on PGE fractionation in the Emeishan picrites and basalts:Constraints from integrated lithophile-siderophile elements and Sr-Nd isotopes. Geochimica et Cosmochimica Acta,90(0):12-32.
Lifshitz, I.M. and Slyozov, V.V.,1961. The kinetics of precipitation from supersaturated solid solutions. Journal of Physics and Chemistry of Solids,19(1-2):35-50.
Lightfoot, P.C., Hawkesworth, C.J., Hergt, J., Naldrett, A.J., Gorbachev, N.S., Fedorenko, V.A. and Doherty, W.,1993. Remobilisation of the continental lithosphere by a mantle plume: major-, trace-element, and Sr-, Nd-, and Pb-isotope evidence from picritic and tholeiitic lavas of the Noril'sk District, Siberian Trap, Russia. Contributions to Mineralogy and Petrology,114(2):171-188.
Li, Y.G., Ma, Y, Ji, X., Li, J., Huang, M. and Min, Z.,2003. Mineral resources of Panzhihua, Sichuan Province, S W China. Chengdu University of Technology,275.
Lo, C.H., Chung, S.L., Lee, T.Y. and Wu, G,2002. Age of the Emeishan flood magmatism and relations to Permian-Triassic boundary events. Earth and Planetary Science Letters,198(3):449-458.
Magee, C, O'driscoll, B. and Chambers, A.D.,2010. Crystallization and textural evolution of a closed-system magma chamber:insights from a crystal size distribution study of the Lilloise layered intrusion, East Greenland. Geological Magazine,147(03):363-379.
Melluso, L., Mahoney, J.J. and Dallai, L.,2006. Mantle sources and crustal input as recorded in high-Mg Deccan Traps basalts of Gujarat (India). Lithos,89(3-4):259-274.
Marsh, B.D.,1981. On the crystallinity, probability of occurrence, and rheology of lava and magma. Contributions to Mineralogy and Petrology,78(1):85-98.
Marsh, B.D.,1988. Crystal size distribution (CSD) in rocks and the kinetics and dynamics of crystallization. Contributions to Mineralogy and Petrology,99(3):277-291.
Marsh, B.D.,1996. Solidification fronts and magmatic evolution. Mineralogical Magazine,60(1):5-40.
Marsh, B.D.,1998. On the Interpretation of Crystal Size Distributions in Magmatic Systems. Journal of Petrology,39(4):553-599.
Martin, V.M., Davidson, J., Morgan, D. and Jerram, D.A.,2010. Using the Sr isotope compositions of feldspars and glass to distinguish magma system components and dynamics. Geology,38(6):539-542.
Melnik, O. and Sparks, R.S.I.,2002. Dynamics of magma ascent and lava extrusion at Soufriere Hills Volcano, Montserrat. Geological Society,21:153-171
Miller, J.S. and Wooden, J.L.,2004. Residence,resorption and recycling of zicons in Devils Kitchen Rhyolite,Coso Volcanic Field,California. J. Petrology,45(11):2155-2170
Mills, R.D., Ratner, J.J. and Glazner, A.F.,2011. Experimental evidence for crystal coarsening and fabric development during temperature cycling. Geology,39(12):1139-1142.
Mock, A. and Jerram, D.A.,2005. Crystal Size Distributions (CSD) in Three Dimensions:Insights from the3D Reconstruction of a Highly Porphyritic Rhyolite. Journal of Petrology,46(8):1525-1541.
Molloy, C, Shane, Phil, and Nairn, Ⅰ,2008. Pre-eruption thermal rejuvenation and stirring of a partly crystalline rhyolite pluton revealed by the Earthquake Flat Pyroclastics deposit, New Zealand. Journal of the Geological Society,165:435-447
Morgan, D.J. and Jerram, D.A.,2006. On estimating crystal shape for crystal size distribution analysis. Journal of Volcanology and Geothermal Research,154(1-2):1-7.
Morgan, D.J., Jerram, D.A., Chertkoff, D.G., Davidson, J.P., Pearson, D.G., Kronz, A. and Nowell, G.M.,2007. Combining CSD and isotopic microanalysis:Magma supply and mixing processes at Stromboli Volcano, Aeolian Islands, Italy. Earth and Planetary Science Letters,260(3-4):419-431.
Morgan, W.J.,1971. Convection Plumes in the Lower Mantle. Nature,230(5288):42-43.
Pang, K.-N., Li, C, Zhou, M.-F. and Ripley, E.,2008a. Abundant Fe-Ti oxide inclusions in olivine from the Panzhihua and Hongge layered intrusions, SW China:evidence for early saturation of Fe-Ti oxides in ferrobasaltic magma. Contributions to Mineralogy and Petrology,156(3):307-321.
Pang, K.N., Li, C, Zhou, M.F. and Ripley, E.M.,2009. Mineral compositional constraints on petrogenesis and oxide ore genesis of the late Permian Panzhihua layered gabbroic intrusion, SW China. Lithos,110(1-4):199-214.
Pang, K.N., Zhou, M.F., Lindsley, D., Zhao, D. and Malpas, J.,2008b. Origin of Fe-Ti Oxide Ores in Mafic Intrusions:Evidence from the Panzhihua Intrusion, SW China. Journal of Petrology,49(2):295-313.
Parsons, I.,1987. Origins of igneous layering. Springer.
Patwardhan, K. and Marsh, B.D.,2011. Dynamics of the Development of the Isle au Haut Gabbro-Diorite Layered Complex:Quantitative Implications for Mafic-Silicic Magma Interactions. Journal of Petrology,52(12):2365-2395.
Pearce, J. and Norry, M.,1979. Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks. Contributions to Mineralogy and Petrology,69(1):33-47.
Peate, D.W, Hawkesworth, C.J., Mantovani, M.M., Rogers, N.W and Turner, S.P.,1999. Petrogenesis and stratigraphy of the high-Ti/Y Urubici magma type in the Parana flood basalt province and implications for the nature of'Dupal'-type mantle in the South Atlantic region. Journal of Petrology,40(3):451-473.
Pik, R., Deniel, C, Coulon, C, Yirgu, G., Hofmann, C. and Ayalew, D.,1998. The northwestern Ethiopian Plateau flood basalts:classification and spatial distribution of magma types. Journal of Volcanology and Geothermal Research,81(1):91-111.
Putirka, K.D.,2005. Igneous thermometers and barometers based on plagioclase＋liquid equilibria:Tests of some existing models and new calibrations. American Mineralogist,90(2-3):336-346.
Putirka, K.D.,2008. Thermometers and Barometers for Volcanic Systems. Reviews in Mineralogy and Geochemistry,69(1):61-120.
Ramos, F.C., Wolff, J.A. and Tollstrup, D.L.,2004. Measuring87Sr/86Sr variations in minerals and groundmass from basalts using LA-MC-ICPMS. Chemical Geology,211(1-2):135-158.
Revillon, S., Arndt, N., Hallot, E., Kerr, A. and Tarney, J.,1999. Petrogenesis of picrites from the Caribbean Plateau and the North Atlantic magmatic province. Lithos,49(1):1-21.
Salisbury, M.J., Bohrson, W.A., Clynne, M.A., Ramos, E.C. and Hoskin, P.,2008. Multiple Plagioclase Crystal Populations Identified by Crystal Size Distribution and in situ Chemical Data:Implications for Timescales of Magma Chamber Processes Associated with the1915Eruption of Lassen Peak, CA. Journal of Petrology,49(10):1755-1780.
Scarfe, C.M., Cronin, D.J., Wenzel, J.T. and Kauffman, D.A.,1983. Viscosity-temperature relationships at1atm in the system diopside-anorthite. Amer. Mineral.68,1083-1088
Sen, G.,2001. Generation of Deccan Trap magmas. J Earth Syst Sci,110(4):409-431.
Shane, P., Martin, S.B., Smith, V.C., Beggs, K.F., Darragh, M.B., Cole, J.W. and Nairn,I.A.2007. Multiple rhyolite magmas and basalt injection in the17.7ka Rerewhakaaitu eruption episode from Tarawera volcanic complex, New Zealand. Journal of Volcanology and Geothermal Research,164:1-26
Shaw, H.R.,1972.Viscosities of magmatic silicate liquids:An empirical method of prediction,Am.J. Sci,272:870-893
Shellnutt, J.G. and Jahn, B.M.,2010. Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex:Implications for the genesis of Fe-Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters,289(3-4):509-519.
Shellnutt, J.G, Wang, K.L., Zellmer, G.F., Iizuka, Y., Jahn, B.M., Pang, K.N., Qi, L. and Zhou, M.F.,2011. Three Fe-Ti oxide ore-bearing gabbro-granitoid complexes in the Panxi region of the Permian Emeishan large igneous province, SW China. American Journal of Science,311(9):773-812.
Shellnutt, J., Zhou, M.F., Yan, D.P. and Wang, Y.B.,2008. Longevity of the Permian Emeishan mantle plume (SW China):1Ma,8Ma or18Ma? Geological Magazine,145(3):373-388.
Shellnutt, J.G., Zhou, M.F. and Zellmer, G.F.,2009. The role of Fe-Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap:An example from the Permian Baima igneous complex, SW China. Chemical Geology,259(3-4):204-217.
Shellnutt, J.G., Denyszyn, S.W. and Mundil, R.,2012. Precise age determination of mafic and felsic intrusive rocks from the Permian Emeishan large igneous province (SW China). Gondwana Research,22(1):118-126.
Simakin, A.G. and Bindeman, I.N.,2008. Evolution of crystal sizes in the series of dissolution and precipitation events in open magma systems. Journal of Volcanology and Geothermal Research,177(4):997-1010.
Sobolev, A.V., Hofmann, A.W., Kuzmin, D.V., Yaxley, G.M., Arndt, N.T., Chung, S.-L. Danyushevsky, L.V., Elliott, T., Frey, F.A., Garcia, M.O., Gurenko, A.A., Kamenetsky, V.S., Kerr, A.C., Krivolutskaya, N.A., Matvienkov, V.V., Nikogosian, I.K., Rocholl, A., Sigurdsson, I.A., Sushchevskaya, N.M. and Teklay, M.,2007. The Amount of Recycled Crust in Sources of Mantle-Derived Melts. Science,316(5823):412-417.
Solano, J.M.S., Jackson, M.D., Sparks, R.S.J., Blundy, J.D. and Annen, C.,2012. Melt Segregation in Deep Crustal Hot Zones:a Mechanism for Chemical Differentiation, Crustal Assimilation and the Formation of Evolved Magmas. Journal of Petrology,53(10):1999-2026.
Song, X.Y., Zhou, M.F., Cao, Z.M., Sun, M. and Wang, Y.L.,2003. Ni-Cu-(PGE) magmatic sulfide deposits in the Yangliuping area, Permian Emeishan igneous province, SW China. Miner Deposita,38(7):831-843.
Song, X.Y, Zhou, M.F., Hou, Z.Q., Cao, Z.-M., Wang, Y.-L. and Li, Y.,2001. Geochemical Constraints on the Mantle Source of the Upper Permian Emeishan Continental Flood Basalts, Southwestern China. International Geology Review,43(3):213-225.
Sun, S.S. and McDonough, W.F.,1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. Geological Society, London, Special Publications,42(1):313-345.
Suzuki, Y. and Nakada, S.,2007. Remobilization of highly crystalline felsic magma by injection of mafic magma:Constraints from the middle sixth century eruption at Haruna volcano, Honshu, Japan. Journal of Petrology,48(8):1543-1567.
Tao, Y., Li, C, Song, X.Y. and Ripley, E.,2008. Mineralogical, petrological, and geochemical studies of the Limahe mafic-ultramatic intrusion and associated Ni-Cu sulfide ores, SW China. Miner Deposita,43(8):849-872.
Taylor, S.R. and McLennan, S.M.,1985. The continental crust:Its composition and evolution, Medium:X; Size:Pages:328pp.
Ukstins-Peate, I. and Bryan, S.E.,2008. Re-evaluating plume-induced uplift in the Emeishan large igneous province. Nature Geosci,1(9):625-629.
Vance, J.,1969. On synneusis. Contributions to Mineralogy and Petrology,24(1):7-29.
Vinet, N. and Higgins, M.D.,2010. Magma Solidification Processes beneath Kilauea Volcano, Hawaii:a Quantitative Textural and Geochemical Study of the1969-1974Mauna Ulu Lavas. Journal of Petrology,51(6):1297-1332.
Wager, L. and Brown, G,1967. Layered Igneous Rocks,588. Oliver and Boyd, San Francisco.
Wagner, C.,1961. Theorie der Alterung von Niederschlagen durch Umlosen (Ostwald-Reifung). Zeitschrift fur Elektrochemie, Berichte der Bunsengesellschaft fur physikalische Chemie,65(7-8):581-591.
Wang, C, Zhou, M.F. and Keays, R.,2006. Geochemical constraints on the origin of the Permian Baimazhai mafic-ultramafic intrusion, SW China. Contributions to Mineralogy and Petrology,152(3):309-321.
Wang, C.Y., Zhou, M.F. and Qi, L.,2007. Permian flood basalts and mafic intrusions in the Jinping (SW China)-Song Da (northern Vietnam) district:Mantle sources, crustal contamination and sulfide segregation. Chemical Geology,243(3-4):317-343.
Wang, C, Zhou, M.F., Sun, Y. and Arndt, N.,2012. Differentiation, crustal contamination and emplacement of magmas in the formation of the Nantianwan mafic intrusion of the-260Ma Emeishan large igneous province, SW China. Contributions to Mineralogy and Petrology,164(2):281-301.
Wang, C.Y., Zhou, M.F. and Zhao, D.,2005. Mineral chemistry of chromite from the Permian Jinbaoshan Pt-Pd-sulphide-bearing ultramafic intrusion in SW China with petrogenetic implications. Lithos,83(1):47-66.
Wang, K., Plank, T., Walker, J.D., et al.,2002. A mantle melting profile across the Basin and Range,SWUSA. Journal of Geophysical Research,107(B1),doi:10.1029/2001JB000209
Wang, Y., Zhang, X.M., Jiang, C.S., Wei, H.Q. and Wan, J.L.,2007. Tectonic controls on the late Miocene-Holocene volcanic eruptions of the Tengchong volcanic field along the southeastern margin of the Tibetan plateau. Journal of Asian Earth Sciences,30:375-389
Wiebe, R.A., Manon, M.R., Hawkins, D.P. and McDonough, W.F.,2004. Late-stage mafic injection and thermal rejuvenation of the Vinalhaven granite, Coastal Maine. Journal of Petrology,45(11):2133-2153
Williams, E., Boudreau, A.E., Boorman, S. and Kruger, F.J.,2006. Textures of orthopyroxenites from the Burgersfort bulge of the eastern Bushveld Complex, Republic of South Africa. Contributions to Mineralogy and Petrology,151(4):480-492.
Wilson, J.T.,1963. A POSSIBLE ORIGIN OF THE HAWAIIAN ISLANDS. Canadian Journal of Physics,41(6):863-870.
Xiao, L., Xu, Y.G., Mei, H.J., Zheng, Y.F., He, B. and Pirajno, F.,2004. Distinct mantle sources of low-Ti and high-Ti basalts from the western Emeishan large igneous province, SW China: implications for plume-lithosphere interaction. Earth and Planetary Science Letters,228(3-4):525-546.
Xu, Y.G., Chung, S.L., Shao, H. and He, B.,2010. Silicic magmas from the Emeishan large igneous province, Southwest China:Petrogenesis and their link with the end-Guadalupian biological crisis. Lithos,119(1-2):47-60.
Xu, Y.G., He, B., Chung, S.L., Menzies, M.A. and Frey, F.A.,2004. Geologic, geochemical, and geophysical consequences of plume involvement in the Emeishan flood-basalt province. Geology,32(10):917-920.
Xu, Y.G., Luo, Z.Y., Huang, X.L., He, B., Xiao, L., Xie, L.W and Shi, Y.R.,2008. Zircon U-Pb and Hf isotope constraints on crustal melting associated with the Emeishan mantle plume. Geochimicaet Cosmochimica Acta,72(13):3084-3104.
Xu, Y.G., Chung, S.L., Jahn, B.M. and Wu, G.,2001. Petrologic and geochemical constraints on the petrogenesis of Permian-Triassic Emeishan flood basalts in southwestern China. Lithos,58(3-4):145-168.
Yang, Z.F.,2012. Combining Quantitative Textural and Geochemical Studies to Understand the Solidification Processes of a Granite Porphyry:Shanggusi, East Qinling, China. Journal of Petrology,53(9):1807-1835.
Zellmer, G.F., Blake, S., Vance, D., Hawkesworth, C. and Turner, S.,1999. Plagioclase residence times at two island arc volcanoes (Kameni Islands, Santorini, and Soufriere, St. Vincent) determined by Sr diffusion systematics. Contributions to Mineralogy and Petrology,136(4):345-357.
Zellmer, G.F., Sparks, R.S.J., Hawkesworth, C.J. and Wiedenbeck, M.,2003. Magma Emplacement and Remobilization Timescales Beneath Montserrat:Insights from Sr and Ba Zonation in Plagioclase Phenocrysts. J. Petrology,44(8):1413-1431
Zhang, Z., Mahoney, J.J., Mao, J. and Wang, F.,2006. Geochemistry of Picritic and Associated Basalt Flows of the Western Emeishan Flood Basalt Province, China. Journal of Petrology,47(10):1997-2019.
Zhang, Z., Mao, J., Saunders, A.D., Ai, Y., Li, Y. and Zhao, L.,2009. Petrogenetic modeling of three mafic-ultramafic layered intrusions in the Emeishan large igneous province, SW China, based on isotopic and bulk chemical constraints. Lithos,113(3-4):369-392.
Zhang, Z., Zhi, X., Chen, L., Saunders, A.D. and Reichow, M.K.,2008. Re-Os isotopic compositions of picrites from the Emeishan flood basalt province, China. Earth and Planetary Science Letters,276(1-2):30-39.
Zhong, H., Qi, L., Hu, R.Z., Zhou, M.F., Gou, T.Z., Zhu, W.G., Liu, B.G. and Chu, Z.Y.,2011. Rhenium-osmium isotope and platinum-group elements in the Xinjie layered intrusion, SW China:Implications for source mantle composition, mantle evolution, PGE fractionation and mineralization. Geochimica et Cosmochimica Acta,75(6):1621-1641.
Zhong, H., Yao, Y, Prevec, S.A., Wilson, A.H., Viljoen, M.J., Viljoen, R.P., Liu, B.-G. and Luo, Y.-N.,2004. Trace-element and Sr-Nd isotopic geochemistry of the PGE-bearing Xinjie layered intrusion in SW China. Chemical Geology,203(3-4):237-252.
Zhong, H., Zhu, W.G., Hu, R.Z., Xie, L.W, He, D.F., Liu, F. and Chu, Z.Y.,2009. Zircon U-Pb age and Sr-Nd-Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust. Lithos,110(1-4):109-128.
Zhong, Y.T., He, B,, Mundil, R., Xu, Y.G.2014. CA-TIMS zircon U-Pb dating of felsic ignimbrite from the Binchuan section:Implications for the termination age of Emeishan large igneous province. Lithos,10.1016/j.lithos.2014.03.005
Zhou, M.F., Arndt, N.T., Malpas, J., Wang, C.Y. and Kennedy, A.K.,2008. Two magma series and associated ore deposit types in the Permian Emeishan large igneous province, SW China. Lithos,103(3):352-368.
Zhou, M.F., Chen, W.T., Wang, C.Y., Prevec, S.A., Liu, Patricia P. and Howarth, G.H.,2013. Two stages of immiscible liquid separation in the formation of Panzhihua-type Fe-Ti-V oxide deposits, SW China. Geoscience Frontiers,4(5):481-502.
Zhou, M.F., Malpas, J., Song, X.Y., Robinson, P.T., Sun, M., Kennedy, A.K., Lesher, C.M. and Keays, R.R.,2002. A temporal link between the Emeishan large igneous province (SW China) and the end-Guadalupian mass extinction. Earth and Planetary Science Letters,196(3-4):113-122.
Zhou, M.F., Robinson, P.T., Lesher, C.M., Keays, R.R., Zhang, C.-J. and Malpas, J.,2005. Geochemistry, Petrogenesis and Metallogenesis of the Panzhihua Gabbroic Layered Intrusion and Associated Fe-Ti-V Oxide Deposits, Sichuan Province, SW China. Journal of Petrology,46(11):2253-2280.
Zhu, B., Guo, Z., Liu, R., Liu, D. and Du, W.,2014. No pre-eruptive uplift in the Emeishan large igneous province:New evidences from its'inner zone', Dali area, Southwest China. Journal of Volcanology and Geothermal Research,269(0):57-67.
Zhu, B.Q., Mao, C.X., Lugmair, G.W. and Macdougall, J.D.,1983. Isotopic and geochemical evidence for the origin of Plio-Pleistocene volcanic rocks near the Indo2Eurasian collisional margin at Tengchong, China[J]. Earth Planet. Sci. Lett.65(2):263-275.
Zieg, M.J. and Marsh, B.D.,2002. Crystal Size Distributions and Scaling Laws in the Quantification of Igneous Textures. Journal of Petrology,43(1):85-101.
何斌,徐义刚,肖龙等.2006.峨眉山地幔柱上升的沉积相应及其地质意义.地质论评,52(1)：30-37
侯增谦,卢记仁,汪云亮,夏林圻,李红阳和国连杰,1999.峨眉火成岩省：结构、成因与特色.地质论评(S1)：885-891.
皇甫岗,石绍先,苏有锦.2000.20世纪云南地震活动研究.地震研究,23(1)：1-9
季建清.1998.腾冲地块西缘岛弧地体中发现洋壳残片.地学前缘,5(3)：50-55
季建清.2000.滇西南新生代走滑断裂运动学、年代学、及对青藏高原东南部块体运动的意义.地质科学,35(3)：336-349
李宏博,张招崇和吕林素,2010.峨眉山大火成岩省基性墙群几何学研究及对地幔柱中心的指示意义.岩石学报(10)：3143-3152.
李廷栋.2010.中国岩石圈的基本特征.地学前缘,17(3)：2-13
李佑国.2007.基于“3S”技术的攀西地区铜镍铂族元素矿床找靶筛选[C].成都：成都理工大学
梁涛,罗照华,李德东等.2008.托云盆地新生代幔源岩浆源区起止深度的限定.岩石学报,024(11)：2820-2838
梁涛,罗照华,李文韬等.2005.托云火山群的火山地质特征及其构造意义.新疆地质,23(2)：105-110
刘杕,沈发奎,张光宗.攀西地区层状岩体[A].张云湘主编.中国攀西裂谷文集[C].北京：地质出版社,1985：85-118
罗照华,辛后田,陈必河,柯珊和黄金香.2007.壳幔过渡层及其大陆动力学意义.现代地质,21(2)：421-425
罗照华,莫宣学,侯增谦等.2006.青藏高原新生代形成演化的整合模型——来自火成岩的约束.地学前缘,13(4)：196-211
罗照华,卢欣祥,郭少丰,孙静,陈必河,黄凡和杨宗锋.2008a.透岩浆流体成矿体系.岩石学报(12)：2669-2678.
罗照华,卢欣祥,刘翠,李德东,杨宗锋和文思博.2011.岩浆热液成矿理论的失败：原因和出路.吉林大学学报(地球科学版)(01)：1-11.
罗照华,卢欣祥,王秉璋,陈必河,黄凡,杨宗锋和汪洋.2008b.造山后脉岩组合与内生成矿作用.地学前缘(04)：1-12.
罗照华,刘嘉麒,赵慈平,郭正府,程黎鹿,李晓惠,李大鹏.2010a.深部流体与岩浆活动：兼论腾冲火山群的深部过程。岩石学报,027(10)：2855-62
罗照华,卢欣祥,许俊玉,刘翠,李德东.2010b.成矿侵入体的岩石学标志.岩石学报,026(8)：2247-54
罗照华,莫宣学,卢欣祥,陈必河,柯珊,侯增谦和江万.2007.透岩浆流体成矿作用——理论分析与野外证据.地学前缘(03)：165-183
邱家骧.1991.应用岩浆岩岩石学.中国地质大学出版社.155-158
史仁灯,郝艳丽和黄启帅,2008.Re-Os同位素对峨眉山大火成岩省成因制约的探讨.岩石学报(11)：2515-2523.
宋谢炎,张成江,胡瑞忠等.2005.峨眉火成岩省岩浆矿床成矿作用与地幔柱动力学过程的耦合关系.矿物岩石,25(4)：35-44
汤庆艳,张铭杰,余明,王启立,尚慧,2013.晚二叠世峨眉山地幔柱岩浆成矿作用.岩石矿物学杂志,32(5)：680-692
佟伟,章铭陶.1989.腾冲地热[M].北京：科学出版社.
向才英,周真恒,姜朝松.2000.腾冲火山岩岩石化学研究.云南地质,19(2)：134-151
徐义刚,何斌,黄小龙,罗震宇,朱丹,马金龙和邵辉,2007.地幔柱大辩论及如何验证地幔柱假说.地学前缘(02)：1-9.
云南省地质局.1982.腾冲幅和盈江幅(1：200000)区域地质调查报告.
云南省地质矿产局.1985腾冲幅和朗蒲寨幅(1：50000)区域地质调查报告..
云南省地质矿产局.1992.古永幅(1：50000)区域地质调查报告.
张辉煌,徐义刚,葛文春,等.2006.吉林伊通—大屯地区晚中生代—新生代玄武岩的地球化学特征及其意义.岩石学报,22(6)：1579-1596
赵慈平.2008.腾冲火山区现代幔源氦释放特征及深部岩浆活动你个岩浆.学位论文.
赵志丹,莫宣学,罗照华等.2003.印度—亚洲俯冲带结构—岩浆作用证据.地学前缘,10(3)：149-157
钟宏,徐桂瘟,朱维光等.2009.峨眉山大火成岩省太和花岗岩的成因及构造意义.矿物岩石地球化学通报,28(2)：99-110
周真恒,韩新民,周瑞琦.1996.云南腾冲地区的岩石圈热结构.地震地磁观测与研究,17(4)：34-41
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |