必须声明标量变量 "@Script_ID"。 华北板块东南缘五河杂岩的麻粒岩相变质、部分熔融与交代作用-《地球科学与环境学报》
|本期目录/Table of Contents|

[1]刘贻灿,王程程,张品刚,等.华北板块东南缘五河杂岩的麻粒岩相变质、部分熔融与交代作用[J].地球科学与环境学报,2015,37(01):1-11.
 LIU Yi-can,WANG Cheng-cheng,ZHANG Pin-gang,et al.Granulite Facies Metamorphism, Partial Melting and Metasomatism in the Wuhe Complex at the Southeastern Margin of the North China Block[J].Journal of Earth Sciences and Environment,2015,37(01):1-11.
点击复制

华北板块东南缘五河杂岩的麻粒岩相变质、部分熔融与交代作用(PDF)
分享到:

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第37卷
期数:
2015年第01期
页码:
1-11
栏目:
基础地质与矿产地质
出版日期:
2015-01-15

文章信息/Info

Title:
Granulite Facies Metamorphism, Partial Melting and Metasomatism in the Wuhe Complex at the Southeastern Margin of the North China Block
文章编号:
1672-6561(2015)01-0001-11
作者:
刘贻灿王程程张品刚GROPPO ChiaraROLFOFranco王安东
1. 中国科学院壳幔物质与环境重点实验室,安徽 合肥 230026; 2. 中国科学技术大学 地球和空间科学学院,安徽 合肥 230026; 3. 安徽省煤田地质局勘查研究院,安徽 合肥 230088; 4. 都灵大学 地球科学系,皮埃蒙特 都灵 10124
Author(s):
LIU Yi-canWANG Cheng-chengZHANG Pin-gangGROPPO ChiaraROLFO FrancoWANG An-dong
1. Key Laboratory of Crust-mantle Materials and Environments, Chinese Academy of Sciences, Hefei 230026, Anhui, China; 2. School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, Anhui, China; 3. Exploration Institute of Anhui Coalfield Geology Bureau, Hefei 230088, Anhui, China; 4. Department of Earth Sciences, University of Torino, Torino 10124, Piedmont, Italy
关键词:
麻粒岩相多阶段变质作用部分熔融交代作用前寒武纪五河杂岩华北板块
Keywords:
granulite facies multistage metamorphism partial melting metasomatism Precambrian Wuhe complex North China Block
分类号:
P588.3
DOI:
-
文献标志码:
A
摘要:
华北板块东南缘五河杂岩属于前寒武纪变质基底,出露于蚌埠及相邻地区,主要由变质的镁铁质和长英质火成岩以及表壳岩系组成,并伴生有古元古代片麻状花岗岩和中生代花岗岩类,构成了“蚌埠隆起”。五河杂岩中主要有石榴斜长角闪岩/榴闪岩、石榴麻粒岩、异剥钙榴岩、石榴斜长角闪片麻岩、花岗片麻岩、云母片岩、大理岩和变质砂岩等岩石类型。这些不同类型的变质岩具有类似的峰期变质矿物,如石榴子石、单斜辉石、斜长石、金红石和石英等;结合其锆石U-Pb年龄,表明它们共同经历了古元古代高压麻粒岩相变质作用。石榴斜长角闪岩的石榴子石包体中存在钾长石+斜长石+石英+黑云母等矿物交生体,指示早期花岗质熔体的存在,证明五河杂岩在古元代变质过程中发生了部分熔融作用。此外,部分变基性岩中存在方解石、绿帘石和绿泥石等蚀变矿物,沿石榴子石的裂隙中分布有钾长石+斜长石+石英+黑云母+角闪石等矿物,表明它们经历了含碳酸盐的熔/流体交代作用以及绿帘石化和绿泥石化作用等。遭受过古元古代含碳酸盐的熔/流体交代作用的变基性岩表现为高放射成因Pb同位素组成,而未遭受含碳酸盐的熔/流体交代作用的变基性岩则表现为典型华北板块前寒武纪麻粒岩地体和下地壳包体岩石的低放射成因Pb同位素组成。
Abstract:
-

参考文献/References:

[1]HARLEY S L.The Origins of Granulites:A MetamorphicPerspective[J].Geological Magazine,1989,126(3):215-247.
[2]GROPPO C,ROLFO F,INDARES A.Partial Melting in the Higher Himalayan Crystallines of Eastern Nepal:The Effect of Decompression and Implications for the‘Channel Flow’Model[J].Journal of Petrology,2012,53(5):1057-1088.
[3]SAWYER E W.Criteria for the Recognition of Partial Melting[J].Physics and Chemistry of the Earth,Part A:Solid Earth and Geodesy,1999,24(3):269-279.
[4]SAWYER E W.Melt Segregation in the Continental Crust:Distribution and Movement of Melt in Anatectic Rocks[J].Journal of Metamorphic Geology,2001,19(3):291-309.
[5]VILLASECA C,ROMERA C M,BARBERO L.Melts and Residua Geochemistry in a Low-to-mid Crustal Section(Central Spain)[J].Physics and Chemistry of the Earth,Part A:Solid Earth and Geodesy,2001,26(4/5):273-280.
[6] BROWN M.The Generation,Segregation,Ascent and Emplacement of Granite Magma:The Migmatite-tocrustally-derived Granite Connection in Thickened Orogens[J].Earth-science Reviews,1994,36(1/2):83-130.
[7]BROWN M.The Mechanism of Melt Extraction from Lower Continental Crust of Orogens[J].Transactions of the Royal Society of Edinburgh:Earth Sciences,2004,95(1/2):35-48.
[8]BROWN M.Crustal Melting and Melt Extraction,Ascent and Emplacement in Orogens:Mechanisms and Consequences[J].Journal of the Geological Society,2007,164(4):709-730.
[9]THOMPSON A B.Dehydration Melting of Pelitic Rocks and the Generation of H2O-undersaturated Granitic Liquids[J].American Journal of Science,1982,282(10):1567-1595.
[10]CLEMENS J D,VIELZEUF D.Constraints on Melting and Magma Production in the Crust[J].Earth and Planetary Science Letters,1987,86(2/3/4):287-306.
[11]VIELZEUF D,CLEMENS J D,PIN C,et al.Granites,Granulites,and Crustal Differentiation[M]//VIELZEUFD,VIDAL P.Granulites and Crustal Evolution.Dordrecht:Kluwer Academic Publishers,1990:59-85.
[12]WHITNEY D L,TEYSSIER C,FAYON A K,et al.Tectonic Controls on Metamorphism,Partial Melting,and Intrusion:Timing and Duration of Regional Metamorphism and Magmatism in the Nigde Massif,Turkey[J].Tectonophysics,2003,376(1/2):37-60.
[13]HERMANN J,GREEN D H.Experimental Constraints on High Pressure Melting in Subducted Crust[J].Earth and Planetary Science Letters,2001,188(1/2):149-168.
[14]VANDERHAEGHE O,TEYSSIER C.Partial Melting and Flow of Orogens[J].Tectonophysics,2001,342(3/4):451-472.
[15]ZHONG Z Q,SUO S T,YOU Z D,et al.Major Constituents of the Dabie Collisional Orogenic Belt and Partial Melting in the Ultrahigh-pressure Unit[J].International Geology Review,2001,43(3):226-236.
[16]WHITNEY D L,TEYSSIER C,REY P F.The Consequences of Crustal Melting in Continental Subduction[J].Lithosphere,2009,1(6):323-327.
[17]BROWN M.Melting of the Continental Crust During Orogenesis:The Thermal,Rheological,and Compositional Consequences of Melt Transport from Lower to Upper Continental Crust[J].Canadian Journal of Earth Sciences,2010,47(5):655-694.
[18]LABROUSSE L,PROUTEAU G,GANZHORN A C.Continental Exhumation Triggered by Partial Melting at Ultrahigh Pressure[J].Geology,2011,39(12):1171-1174.
[19]刘贻灿,李曙光,徐树桐,等.北大别片麻岩的超高压变质证据:来自锆石提供的信息[J].岩石学报,2006,22(7):1827-1832.[LIU Yi-can,LI Shu-guang,XU Shu-tong,et al.Ultrahigh-pressure Metamorphic Evidence for Gneiss from the Northern Dabie Complex,Central China:Message from Zircon[J].Acta Petrologica Sinica,2006,22(7):1827-1832.]
[20]刘贻灿,李 远,刘理湘,等.大别造山带三叠纪低级变质的新元古代火成岩:俯冲陆壳表层拆离折返的岩片[J].科学通报,2013,58(23):2330-2337.[LIU Yi-can,LI Yuan,LIU Li-xiang,et al.Neoproterozoic Low-grade Metagranites and Metabasites in the Dabie Orogen:Implications for Detachment of Subducted Continental Crust at Shallow Depths[J].Chinese Science Bulletin,2013,58(23):2330-2337.]
[21]古晓锋,刘贻灿,邓亮鹏.北大别罗田榴辉岩的同位素年代学和岩石成因及其在折返过程中的元素和同位素行为[J].科学通报,2013,58(22):2132-2137.[GU Xiao-feng,LIU Yi-can,DENG Liang-peng.Geochronology and Petrogenesis of Eclogite from the Luotian Dome,North Dabie Complex Zone(Central China),and Their Element and Isotope Behavior During Exhumation[J].Chinese Science Bulletin,2013,58(22):2132-2137.]
[22]刘贻灿,古晓锋,邓亮鹏.北大别的高温超高压变质作用与多阶段折返[J].岩石学报,2011,27(2):589-600.
[LIU Yi-can,GU Xiao-feng,DENG Liang-peng.High-T/UHP Metamorphism and Multistage Exhumation History of the North Dabie Complex Zone[J].Acta Petrologica Sinica,2011,27(2):589-600.]
[23]刘贻灿,刘理湘,古晓锋,等.大别山北淮阳带西段新元古代浅变质花岗岩的发现及其大地构造意义[J].科学通报,2010,55(24):2391-2399.[LIU Yi-can,LIU Li-xiang,GU Xiao-feng,et al.Occurrence of Neoproterozoic Low-grade Metagranite in the Western Beihuaiyang Zone,the Dabie Orogen[J].Chinese Science Bulletin,2010,55(24):2391-2399.]
[24]刘贻灿,古晓锋,李曙光.北大别超高压榴辉岩的快速折返与缓慢冷却过程[J].岩石学报,2009,25(9):2149-2156.[LIU Yi-can,GU Xiao-feng,LI Shu-guang.Rapid Exhumation and Slow Cooling of Ultrahigh-pressure Eclogite in the North Dabie Complex Zone,Central China[J].Acta Petrologica Sinica,2009,25(9):2149-2156.]
[25]WEBER M B I,TARNEY J,KEMPTON P D,et al.Crustal Make-up of the Northern Andes:Evidence Based on Deep Crustal Xenolith Suites,Mercaderes,SW Colombia[J].Tectonophysics,2002,345(1/2/3/4):49-82.
[26]PATTISON D R M.Petrogenetic Significance of Orthopyroxene-free Garnet + Clinopyroxene + Plagioclase ± Quartz-bearing Metabasites with Respect to the Amphibolite and Granulite Facies[J].Journal ofMetamorphic Geology,2003,21(1):21-34.
[27]YARDLEY B W D.An Introduction to Metamorphic Petrology[M].Englewood Cliffs:Prentice Hall,1989.
[28]O’BRIEN P J,ROTZLER J.High-pressure Granulites:Formation,Recovery of Peak Conditions and Implications for Tectonics[J].Journal of Metamorphic Geology,2003,21(1):3-20.
[29]INDARES A D.Metamorphic Textures and P-T Evolution of High-P Granulites from the Lelukuau Terrane,NE Grenville Province[J].Journal of Metamorphic Geology,2003,21(1):35-48.
[30]ZHAO G C,WILDE S A,CAWOOD P A,et al.Archean Blocks and Their Boundaries in the North China Craton:Lithological,Geochemical,Structural,and P-T Path Constraints and Tectonic Evolution[J].Precambrian Research,2001,107(1/2):45-73.
[31]LIU Y,ZHONG D.Petrology of High-pressure Granulites from the Eastern Himalayan Syntaxis[J].Journal of Metamorphic Geology,1997,15(4):451-466.
[32]CARSWELL D A,O’BRIEN P J.Thermobarometry and Geotectonic Significance of High-pressure Granulites:Examples from the Moldanubian Zone of the Bohemian Massif in Lower Austria[J].Journal of Petrology,1993,34(3):427-459.
[33]ZHAO G C,CAWOOD P A,WILDE S A,et al.Metamorphism of Basement Rocks in the Central Zone of the North China Craton:Implications for Paleoproterozoic Tectonic Evolution[J].Precambrian Research,2000,103(1/2):55-88.
[34]ZHAO G C,SUN M,WILDE S A,et al.Late Archean to Paleoproterozoic Evolution of the North China Craton:Key Issues Revisited[J].Precambrian Research,2005,136(2):177-202.
[35]GUO J H,O’BRIEN P J,ZHAI M.High-pressure Granulites in the Sanggan Area,North China Craton:Metamorphic Evolution,P-T Paths and Geotectonic Significance[J].Journal of Metamorphic Geology,2002,20(8):741-756.
[36]GUO J H,SUN M,CHEN F K,et al.Sm-Nd and SHRIMP U-Pb Zircon Geochronology of High-pressure Granulites in the Sanggan Area,North China Craton:Timing of Paleoproterozoic Continental Collision[J].Journal of Asian Earth Sciences,2005,24(5):629-642.
[37]WILDE S A,ZHAO G C,SUN M.Development of the North China Craton During the Late Archaean and Its Final Amalgamation at 1.8Ga:Some Speculations on Its Position Within a Global Palaeoproterozoic Supercontinent[J].Gondwana Research,2002,5(1):85-94.
[38]KRONER A,WILDE S A,LI J H,et al.Age and Evolution of a Late Archean to Paleoproterozoic Upper to Lower Crustal Section in the Wutaishan/Hengshan/Fuping Terrain of Northern China[J].Journal of Asian Earth Sciences,2005,24(5):577-595.
[39]WILDE S A,ZHAO G C.Late Archean to Paleoproterozoic Evolution of the North China Craton[J].Journal of Asian Earth Sciences,2005,24(5):519-522.
[40]HOU G T,LIU Y L,LI J H.Evidence for~1.8Ga Extension of the Eastern Block of the North China Craton from SHRIMP U-Pb Dating of Mafic Dyke Swarms in Shandong Province[J].Journal of Asian Earth Sciences,2006,27(4):392-401.
[41]翟明国,卞爱国.华北克拉通新太古代末超大陆拼合及古元古代末—中元古代裂解[J].中国科学:D辑,地球科学,2000,30(增):129-137.[ZHAI Ming-guo,BIAN Ai-guo.The Amalgamation of the Supercontinent of North China Craton at the End of Neoarchaean and Its Breakup During Late Palaeoproterozoic and Mesoproterozoic[J].Science in China:Series D,Earth Sciences,2000,30(S):129-137.]
[42]ZHAI M G,LIU W J.Palaeoproterozoic Tectonic History of the North China Craton:A Review[J].Precambrian Research,2003,122(1/2/3/4):183-199.
[43]PENG P,ZHAI M G,ZHANG H F,et al.Geochronological Constraints on the Paleoproterozic Evolution of the North China Craton:SHRIMP Zircon Ages of Different Types of Mafic Dikes[J].International Geology Review,2005,47(5):492-508.
[44]HOU G T,LI J H,YANG M H,et al.Geochemical Constraints on the Tectonic Environment of the Late Paleoproterozoic Mafic Dyke Swarms in the North China Craton[J].Gondwana Research,2008,13(1):103-116.
[45]LU S N,ZHAO G C,WANG H C,et al.Precambrian Metamorphic Basement and Sedimentary Cover of theNorth China Craton:A Review[J].Precambrian Research,2008,160(1/2):77-93.
[46]翟明国,郭敬辉,阎月华,等.中国华北太古宙高压基性麻粒岩的发现及初步研究[J].中国科学:B辑,1992,22(12):1325-1330.[ZHAI Ming-guo,GUO Jing-hui,YAN Yue-hua,et al.The Preliminary Study and Discovery of High Pressure Granulites in North China[J].Science in China:Series B,1992,22(12):1325-1330.]
[47]ZHENG J P,SUN M,LU F X,et al.Mesozoic Lower Crustal Xenoliths and Their Significance in Lithospheric Evolution Beneath the Sino-Korean Craton[J].Tectonophysics,2003,361(1/2):37-60.
[48] 刘文军,翟明国,李永刚.胶东莱西地区高压基性麻粒岩的变质作用[J].岩石学报,1998,14(4):449-459.[LIU Wen-jun,ZHAI Ming-guo,LI Yong-gang.Metamorphism of the High-pressure Basic Granulites in Laixi,Eastern Shandong,China[J].Acta Petrologica Sinica,1998,14(4):449-459.]
[49]周喜文,魏春景,耿元生,等.胶北栖霞地区泥质高压麻粒岩的发现及其地质意义[J].科学通报,2004,49(14):1424-1430.[ZHOU Xi-wen,WEI Chun-jing,GENG Yuan-sheng,et al.Discovery and Implications of the High-pressure Pelitic Granulite from the Jiaobei Massif[J].Chinese Science Bulletin,2004,49(14):1424-1430.]
[50]LIU P H,LIU F L,LIU C H,et al.Petrogenesis,PT-t Path,and Tectonic Significance of High-pressure Mafic Granulites from the Jiaobei Terrane,North China Craton[J].Precambrian Research,2013,233:237-258.
[51]郭素淑,李曙光.华北克拉通东南缘古元古代变质和岩浆事件的锆石SHRIMP U-Pb年龄[J].中国科学:D辑,地球科学,2009,39(6):694-699.[GUO Su-shu,LI Shu-guang.SHRIMP Zircon U-Pb Ages for the Paleoproterozoic Metamorphic-magmatic Events in the Southeast Margin of the North China Craton[J].Science in China:Series D,Earth Sciences,2009,39(6):694-699.]
[52]LIU Y C,WANG A D,ROLFO F,et al.Geochronological and Petrological Constraints on Palaeoproterozoic Granulite Facies Metamorphism in Southeastern Margin of the North China Craton[J].Journal of Metamorphic Geology,2009,27(2):125-138.
[53]许文良,王冬艳,刘晓春,等.徐淮地区早侏罗世侵入杂岩体中榴辉岩类包体的发现及其地质意义[J].科学通报,2002,47(8):618-622.[XU Wen-liang,WANG Dong-yan,LIU Xiao-chun,et al.Discovery of Eclogite Inclusions and Its Geological Significance in Early Jurassic Intrusive Complex in Xuzhou-northern Anhui,Eastern China[J].Chinese Science Bulletin,2002,47(8):618-622.]
[54]XU W L,GAO S,WANG Q H,et al.Mesozoic Crustal Thickening of the Eastern North China Craton:Evidence from Eclogite Xenoliths and Petrologic Implications[J].Geology,2006,34(9):721-724.
[55]XU W L,GAO S,YANG D B,et al.Geochemistry of Eclogite Xenoliths in Mesozoic Adakitic Rocks from Xuzhou-Suzhou Area in Central China and Their Tectonic Implications[J].Lithos,2009,107(3/4):269-280.
[56]LIU Y C,WANG A D,LI S G,et al.Composition and Geochronology of the Deep-seated Xenoliths from the Southeastern Margin of the North China Craton[J].Gondwana Research,2013,23(3):1021-1039.
[57]WANG A D,LIU Y C,GU X F,et al.Late-Neoarchean Magmatism and Metamorphism at the Southeastern Margin of the North China Craton and Their Tectonic Implications[J].Precambrian Research,2012,220/221:65-79.
[58]WANG A D,LIU Y C,SANTOSH M,et al.Zircon U-Pb Geochronology,Geochemistry and Sr-Nd-Pb Isotopes from the Metamorphic Basement in the Wuhe Complex:Implications for Neoarchean Active Continental Margin Along the Southeastern North China Craton and Constraints on the Petrogenesis of Mesozoic Granitoids[J].Geoscience Frontiers,2013,4(1):57-71.
[59]LIU D Y,NUTMAN A P,COMPSTON W,et al.Remnants of≥3 800Ma Crust in the Chinese Part of the Sino-Korean Craton[J].Geology,1992,20(4):339-342.
[60]KUSKY T M,LI J H.Paleoproterozoic Tectonic Evolution of the North China Craton[J].Journal of Asian Earth Sciences,2003,22(4):383-397.
[61]王安东,刘贻灿,古晓锋,等.蚌埠老山含石榴子石片麻状花岗岩的锆石SHRIMP U-Pb年龄及其对华南俯冲陆壳再循环的意义[J].矿物岩石,2009,29(2):38-43.[WANG An-dong,LIU Yi-can,GU Xiao-feng,et al.Zircon SHRIMP U-Pb Dating for Garnet-bearing Gneissic Granite at Laoshan,Bengbu:Implications for Recycling of the Subducted Continental Crust of the South China Block[J].Journal of Mineralogy and Petrology,2009,29(2):38-43.]
[62]YANG D B,XU W L,WANG Q H,et al.Chronology and Geochemistry of Mesozoic Granitoids in the Bengbu Area,Central China:Constraints on the Tectonic Evolution of the Eastern North China Craton[J].Lithos,2010,114(1/2):200-216.
[63]PATTISON D R M,CHACKO T,FARQUHAR J,et al.Temperatures of Granulite-facies Metamorphism:Constraints from Experimental Phase Equilibria and Thermobarometry Corrected for Retrograde Exchange[J].Journal of Petrology,2003,44(5):867-900.
[64]VERNON R H,COLLINS W J.Igneous Microstructures in Migmatites[J].Geology,1988,16(12):1126-1129.
[65]HOLNESS M B,SAWYER E W.On the Pseudomorphing of Melt-filled Pores During the Crystallization of Migmatites[J].Journal of Petrology,2008,49(7):1343-1363.
[66]刘贻灿,王安东.华北克拉通东南缘前寒武纪下地壳的幕式生长与多期改造:岩石学?年代学和Hf同位素证据[J].地球科学与环境学报,2012,34(4):1-11.[LIU Yi-can,WANG An-dong.Episodic Growth and Multiple Modification of Precambrian Lower Crust in the Southeastern Margin of North China Craton:Petrologic,Geochronological and Hf-isotopic Evidences[J].Journal of Earth Sciences and Environment,2012,34(4):1-11.]
[67]CESARE B,FERRERO S,SALVIOLI-MARIANI E,et al.“Nanogranite”and Glassy Inclusions:The Anatectic Melt in Migmatites and Granulites[J].Geology,2009,37(7):627-630.
[68]SAWYER E W,CESARE B,BROWN M.When the Continental Crust Melts[J].Elements,2011,7(4):229-234.
[69]FERRERO S,BARTOLI O,CESARE B,et al.Microstructures of Melt Inclusions in Anatectic Metasedimentary Rocks[J].Journal of Metamorphic Geology,2012,30(3):303-322.
[70]BARTOLI O,TAJCMANOVA L,CESARE B,et al.Phase Equilibria Constraints on Melting of Stromatic Migmatites from Ronda(S.Spain):Insights on the Formation of Peritectic Garnet[J].Journal of Metamorphic Geology,2013,31(7):775-789.
[71]COLEMAN R G.Minerals and Rocks:Ophiolites[M].Berlin:Springer-Verlag,1977.
[72]LI X P,RAHN M,BUCHER K.Metamorphic Processes in Rodingites of the Zermatt-SaasOphiolites[J].International Geology Review,2004,46(1):28-51.
[73]FERRANDO S,FREZZOTTI M L,ORIONE P,et al.Late-Alpine Rodingitization in the Bellecombe Metaophiolites(Aosta Valley,Italian Western Alps):Evidence from Mineral Assemblages and Serpentinization-derived H2-bearing Brine[J].International Geology Review,2010,52(10/11/12):1220-1243.
[74]OTHMAN D B,WHITE W M,PATCHETT J.The Geochemistry of Marine Sediments,Island Arc Magma Genesis,and Crust-mantle Recycling[J].Earth and Planetary Science Letters,1989,94(1/2):1-21.
[75]FROST B R,CHACKO T.The Granulite Uncertainty Principle:Limitations on Thermobarometry in Granulites[J].The Journal of Geology,1989,97(4):435-450.
[76]SPEAR F S,FLORENCE F P.Thermobarometry in Granulites:Pitfalls and New Approaches[J].Precambrian Research,1992,55(1/2/3/4):209-241.
[77]DAVIS W J,CANIL D,MACKENZIE J M,et al.Petrology and U-Pb Geochronology of Lower Crustal Xenoliths and the Development of a Craton,Slave Province,Canada[J].Lithos,2003,71(2):541-573.

相似文献/References:

备注/Memo

备注/Memo:
收稿日期:2014-11-10
基金项目:国家自然科学基金项目(41273036);高等学校博士学科点专项科研基金项目(20133402130008)
作者简介:刘贻灿(1962-),男,安徽潜山人,教授,博士研究生导师,理学博士,E-mail:liuyc@ustc.edu.cn。
更新日期/Last Update: 2015-02-04