引文
[1]Collier J D,Helffrich G R.Topography of the“410”and“660”km seismic discontinuities in the Izu-Bonin subductionzone.Geophys.Res.Lett.,1997,24(12):1535-1538.
[2]Ai Y S,Zheng T Y.The upper mantle discontinuitystructure beneath eastern China.Geophys.Res.Lett.,2003,30(21):2089,doi:10.1029/2003GL017678.
[3]许卫卫,郑天愉,赵亮.华北地区410km间断面和660km间断面结构——克拉通活化的地幔动力学状态探测.中国科学:地球科学,2011,41(5):678-685.Xu W W,Zheng T Y,Zhao L.Mantle dynamics of thereactivating North China Craton:Constraints from thetopographies of the 410-km and 660-km discontinuities.Sci.China Ser.D:Earth Sci.,2011,54(6):881-887,doi:10.1007/s11430-010-4163-0.
[4]Lehmann I.S and the structure of the upper mantle.Geophys.J.R.Astron.Soc.,1961,4:124-138.
[5]Vidale J E,Benz H M.Upper-mantle seismic discontinuitiesand the thermal structure of subduction zones.Nature,1992,356(6371):678-683.
[6]Thybo H,Perc'h ucE.The seismic 8°discontinuity andpartial melting in continental mantle.Science,1997,275(5306):1626-1629.
[7]Revenaugh J,Jordan T H.Mantle layering from SCSreverberations 3.The upper mantle.J.Geophys.Res.,1991,96(B12):19781-19810.
[8]Xu F,Vidale J E,Earle P S,et al.Mantle discontinuitiesunder southern Africa from precursors to P′P′df.Geophys.Res.Lett.,1998,25(4):571-574.
[9]Deuss A,Woodhouse J H.The nature of the Lehmanndiscontinuity from its seismological Clapeyron slopes.EarthPlanet.Sci.Lett.,2004,225(3-4):295-304.
[10]Zheng Y C,Lay T,Flanagan M P,et al.Pervasive seismicwave reflectivity and metasomatism of the Tonga mantlewedge.Science,2007,316(5826):855-859.doi:10.1126/science.1138074.
[11]Deuss A.Global observations of mantle discontinuities usingSS and PP precursors.Surv.Geophys.,2009,30(4-5):301-326.doi:10.1007/s10712-009-9078-y.
[12]Deuss A,Woodhouse J H.A systematic search for mantlediscontinuities using SS-precursors.Geophys.Res.Lett.,2002,29(8):1249,doi:1029/2002GL014768.
[13]Williams Q,Revenaugh J.Ancient subduction,mantleeclogite,and the 300 km seismic discontinuity.Geology,2005,33(1):1-4.
[14]Matsukage K N,Nishihara Y,Karato S I.Seismologicalsignature of chemical differentiation of Earth′s upper mantle.J.Geophys.Res.,2005,110:B12305,doi:10.1029/2004JB003504.
[15]Helffrich G.Topography of the transition zone seismicdiscontinuities.Rev.Geophys.,2000,38(1):141-158.
[16]Zang S X,Zhou Y Z,Ning J Y,et al.Multiplediscontinuities near 660km beneath Tonga area.Geophys.Res.Lett.,2006,33:L20312.doi:10.1029/2006GL027262.
[17]Obara K.Hi-net:high sensitivity seismograph network,Japan.//Takanami T,Kitagawa G eds.Lecture Notes inEarth Sciences.Methods and Applications of Signal Processing inSeismic Network Operations.Berlin:Springer,2003,98:79-88.
[18]Kawakatsu H,Watada S.Seismic evidence for deep-watertransportation in the mantle.Science,2007,316(5830):1468-1471.
[19]Zhao D P,Wang Z,Umino N,et al.Tomographic imagingoutside a seismic network:application to the northeast Japanarc.Bull.Seism.Soc.Am.,2007,97(4):1121-1132,doi:10.1785/0120050256.
[20]Engdahl E R,van der Hilst R,Buland R.Global teleseismicearthquake relocation with improved travel times andprocedures for depth determination.Bull.Seism.Soc.Am.,1998,88(3):722-743.
[21]Castle J C,Creager K C.Local sharpness and shear wavespeed jump across the 660-km discontinuity.J.Geophys.Res.,2000,105(B3):6191-6200.
[22]Dziewonski A M,Anderson D L.Preliminary reference Earthmodel.Phys.Earth Planet.Inter.,1981,25(4):297-356.
[23]Kennett B L N,Engdahl E R.Traveltimes for globalearthquake location and phase identification.Geophys.J.Int.,1991,105(2):429-465.
[24]Kennett B L N,Engdahl E R,Buland R.Constraints onseismic velocities in the Earth from traveltimes.Geophys J.Int.,1995,122(1):108-124.
[25]Kanasewich E R,Hemmings C D,Alpaslan T.Nth-rootstack nonlinear multichannel filter.Geophysics,1973,38(2):327-338.
[26]McFadden P L,Drummond B J,Karvis S.The Nth-rootstack:theory,applications,and examples.Geophysics,1986,51(10):1879-1892.
[27]臧绍先,周元泽.N次根倾斜叠加方法在间断面研究中的应用.地球物理学报,2002,45(3):407-415.Zang S X,Zhou Y Z.N-th root slant stack and its applicationin study of mantle discontinuities.Chinese J.Geophys.(inChinese),2002,45(3):407-415.
[28]Rost S,Thomas C.Array seismology:methods andapplications.Rev.Geophys.,2002,40:1008,doi:10.1029/2000RG000100.
[29]Niu F L,Kawakatsu H.Direct evidence for the undulation ofthe 660-km discontinuity beneath Tonga:comparison ofJapan and California array data.Geophys.Res.Lett.,1995,22(5):531-534.
[30]周元泽,臧绍先.牡丹江和海拉尔台下方地幔间断面结构及推论.地球物理学报,2001,44(6):761-773.Zhou Y Z,Zang S X.Mantle discontinuities beneath thestations MDJ and HIA and its implications.Chinese J.Geophys.(in Chinese),2001,46(1):761-773.
[31]Gudmundsson,Sambridge M.A regionalized upper mantle(RUM)seismic model.J.Geophys.Res.,1998,103(B4):7121-7136.
[32]Shearer P M.Upper mantle seismic discontinuities.∥Earth′sDeep Interior:Mineral Physics and Tomography from theAtomic to the Global Scale.AGU Geophysical Monograph,2000,117:115-131.
[33]Collier J D,Helffrich G R,Wood B J.Seismic discontinuitiesand subduction zones.Phys.Earth Planet.Inter.,2001,127(1-4):35-49.
[34]周元泽,眭怡.南美地区下地幔速度界面结构研究.地球物理学报,2010,53(1):86-93.Zhou Y Z,Sui Y.On the velocity interfaces in the lowermantle beneath South America.Chinese J.Geophys.(inChinese),2010,53(1):86-93.
[35]van Keken P E,Hacker B R,Syracuse E M,et al.Subduction factory:4.Depth-dependent flux of H2O fromsubducting slabs worldwide.J.Geophys.Res.,2011,116:B01401,doi:10.1029/2010JB007922.
[36]Akaogi M,Yusa H,Shiraishi K,et al.Thermodynamicproperties ofα-quartz,coesite,and stishovite and equilibriumphase relations at high pressures and high temperatures.J.Geophys.Res.,1995,100(B11):22337-22347.
[37]Liu J,Topor L,Zhang J Z,et al.Calorimetric study of thecoesite-stishovite transformation and calculation of the phaseboundary.Phys.Chem.Miner.,1996,23(1):11-16.
[38]Zhang J Z,Li B S,Utsumi W,et al.In situ X-rayobservations of the coesite-stishovite transition:reversedphase boundary and kinetics.Phys.Chem.Miner.,1996,23(1):1-10.
[39]Angel R J,Chopelas A,Ross N L.Stability of high-densityclinoenstatite at upper-mantle pressures.Nature,1992,358(6384):322-324.
[40]Mendelssohn M J,Price G D.Computer modelling of apressure induced phase change in clinoenstatite pyroxenes.Phys.Chem.Miner.,1997,25(1):55-62.
[41]Woodland A B.The orthorhombic to high-P monoclinic phasetransition in Mg-Fe pyroxenes:can it produce a seismicdiscontinuity?Geophys.Res.Lett.,1998,25(8):1241-1244.
[42]Tibi R,Wiens D A.Detailed structure and sharpness ofupper mantle discontinuities in the Tonga subduction zonefrom regional broadband arrays.J.Geophys.Res.,2005,110:B06313,doi:10.1029/2004JB003433.
[43]刘良,杨家喜,章军锋等.超高压岩石中矿物显微出溶结构研究进展、面临问题与挑战.科学通报,2009,54(10):1387-1400.Liu L,Yang J X,Zhang J F,et al.Exsolution microstructuresin ultrahigh-pressure rocks:Progress,controversies and challenges.Chinese Sci.Bull.,2009,54(12):1983-1995,doi:10.1007/s11434-009-0204-5.
[44]Mibe K,Kawamoto T,Matsukage K N,et al.Slab meltingversus slab dehydration in subduction-zone magmatism.Proc.Natl.Acad.Sci.USA,2011,108(20):8177-8182.