Ali A, Nakamura E, Yamamoto H. 2002. Sm-Nd mineral ages of pegmatite veins and their host rocks from Swat area, Chilas complex, northern Pakistan. J. Asian Earth Sci., 21(3): 331-339.
[2]
Bai L, Zhang T Z. 2015. Complex deformation pattern of the Pamir-Hindu Kush region inferred from multi-scale double-difference earthquake relocations. Tectonophysics, 638: 177-184, doi: 10.1016/j.tecto.2014.11.006.
[3]
Bina C R, Helffrich G. 1994. Phase transition Clapeyron slopes and transition zone seismic discontinuity topography. J. Geophys. Res., 99(B8): 15853-15860.
[4]
Castle J C, Creager K C. 2000. Local sharpness and shear wave speed jump across the 660 km discontinuity. J. Geophys. Res., 105(B3): 6191-6200.
[5]
Collier J D, Helffrich G R. 1997. Topography of the "410" and "660" km seismic discontinuities in the Izu-Bonin Subduction Zone. Geophys. Res. Lett., 24(12): 1535-1538.
[6]
Collier J D, Helffrich G R, Wood B J. 2001. Seismic discontinuities and subduction zones. Phys. Earth Planet. Inter., 127(1-4): 35-49.
[7]
Deuss A. 2009. Global observations of mantle discontinuities using SS and PP precursors. Surv. Geophy., 30(4-5): 301-326.
[8]
Tian X B, Zhao D P, Zhang H S, et al. 2010. Mantle transition zone topography and structure beneath the central Tien Shan orogenic belt. J. Geophys. Res., 115(B10): B10308, doi: 10.1029/2008JB006229.
[9]
Tian X B, Teng J W, Zhang H S, et al. 2011. Structure of crust and upper mantle beneath the Ordos Block and the Yinshan Mountains revealed by receiver function analysis. Phys. Earth Planet. Inter., 184(3-4): 186-193.
[10]
Villaseor A, Spakman W, Engdahl E R. 2003. Influence of regional travel times in global tomographic models. EGS-AGU-EUG Joint Assembly, Abstracts from the meeting held in Nice, France, 6-11 April 2003, abstract 8614.
[11]
Weidner D J, Wang Y B. 2000. Phase transformations: implications for mantle structure. // Karaoto S I, Forte A, Liebermann R, et al., Earth''s Deep Interior: Mineral Physics and Tomography from the Atomic to the Global Scale, Vol. Geophysical Monograph Series 117. American Geophysical Union: 215-235.
[12]
Zang S X, Zhou Y Z. 2002. N-th root slant stack and its application in study of mantle discontinuities. Chinese J. Geophys. (in Chinese), 45(3): 407-415, doi: 10.3321/j.issn:0001-5733.2002.03.012.
[13]
Dziewonski A M, Anderson D L. 1981. Preliminary reference Earth model. Phys. Earth Planet. Inter., 25(4): 297-356.
[14]
Engdahl E R, van der Hilst R, Buland R. 1998. Global teleseismic earthquake relocation with improved travel times and procedures for depth determination. Bull. Seism. Soc. Am., 88(3): 722-743.
[15]
Flanagan M P, Shearer P M. 1998a. Global mapping of topography on transition zone velocity discontinuities by stacking SS precursors. J. Geophys. Res., 103(B2): 2673-2692.
[16]
Flanagan M P, Shearer P M. 1998b. Topography on the 410-km seismic velocity discontinuity near subduction zones from stacking of sS, sP, and pP precursors. J. Geophys. Res., 103(B9): 21165-21182.
[17]
Fukao Y, Obayashi M. 2013. Subducted slabs stagnant above, penetrating through, and trapped below the 660 km discontinuity. J. Geophys. Res., 118(11): 5920-5938.
[18]
Gudmundsson , Sambridge M. 1998. A regionalized upper mantle (RUM) seismic model. J. Geophys. Res., 103(B4): 7121-7136.
[19]
Jin Z M, Zhang Z J, Wu Y, et al. 2013. Mantle transition zone and research methods. // Ding Z L ed. Research Methods in Solid Earth (in Chinese). Beijing: Science Publishing Company: 402-434.
[20]
Kanasewich E R, Hemmings C D, Alpaslan T. 1973. Nth-root stack nonlinear multichannel filter. Geophysics, 38(2): 327-338.
[21]
Kennett B L N, Engdahl E R. 1991. Traveltimes for global earthquake location and phase identification. Geophys. J. Int., 105(2): 429-465.
[22]
Kennett B L N, Engdahl E R, Buland R. 1995. Constraints on seismic velocities in the Earth from traveltimes. Geophys. J. Int., 122(1): 108-124.
[23]
Koulakov I, Sobolev S V. 2006. A tomographic image of Indian lithosphere break-off beneath the Pamir-Hindu Kush region. Geophys. J. Int., 164(2): 425-440.
[24]
Li X, Sobolev S V, Kind R, et al. 2000. A detailed receiver function image of the upper mantle discontinuities in the Japan subduction zone. Earth Planet. Sci. Lett., 183(3-4): 527-541.
[25]
McFadden P L, Drummond B J, Karvis S. 1986. The N-th root stack: theory, application and examples. Geophysics, 51(10): 1879-1892.
[26]
Negredo A M, Replumaz A, Villaseor A, et al. 2007. Modeling the evolution of continental subduction processes in the Pamir-Hindu Kush region. Earth Planet. Sci. Lett., 259(1-2): 212-225.
[27]
Ning J Y, Zang S X. 1990. The distribution of Earthquakes and Stress State in Pamir-Hindu Kush Regions. Chinese J. Geophys. (in Chinese), 33(6): 657-669.
[28]
Obayashi M, Sugioka H, Yoshimitsu J, et al. 2006. High temperature anomalies oceanward of subducting slabs at the 410 km discontinuity. Earth Planet. Sci. Lett., 243(1-2): 149-158.
[29]
Pegler G, Das S. 1998. An enhanced image of the Pamir-Hindu Kush seismic zone from relocated earthquake hypocentres. Geophys. J. Int., 134(2): 573-595.
[30]
Revenaugh J, Jordan T H. 1991. Mantle layering from ScS reverberations: 1. Waveform inversion of zeroth-order reverberations. J. Geophys. Res., 96(B12): 19749-19762.
[31]
Rost S, Thomas C. 2002. Array seismology: methods and applications. Rev. Geophys., 40(3): 2-1—2-27, doi: 10.1029/2000RG000100.
[32]
Sippl C, Schurr B, Yuan X, et al. 2013. Geometry of the Pamir-Hindu Kush intermediate-depth earthquake zone from local seismic data. J. Geophys. Res., 118(4): 1438-1457.
[33]
Song T R A, Helmberger D V, Grand S P. 2004. Low-velocity zone atop the 410-km seismic discontinuity in the northwestern United States. Nature, 427(6974): 530-533.
[34]
Sun W B, He Y S, Chang Z, et al. 2009. The plate subduction and stress state in the Pamir-Hindu Kush region. Seism. Geol. (in Chinese), 31(2): 207-217.
[35]
Zang S X, Zhou Y Z, Ning J Y, et al. 2006. Multiple discontinuities near 660 km beneath Tonga area. Geophys. Res. Lett., 33(20): L20312, doi: 10.1029/2006GL027262.
[36]
Zhang L P, Shao Z G, Li Z H. 2014. Dynamic action of mutual subduction between the Indian and the Eurasia plates in Hindu Kush-Pamir region. Chinese J. Geophys. (in Chinese), 57(2): 459-471, doi: 10.6038/cjg20140212.
[37]
Zhang Z J, Yuan X H, Chen Y, et al. 2010. Seismic signature of the collision between the east Tibetan escape flow and the Sichuan Basin. Earth Planet. Sci. Lett., 292(3-4): 254-264.
