| [1] Leeds A R, Knopoff L, Kausel E G. Variations of upper mantle structure under the pacific ocean[J]. Science, 1974, 186: 141-143.[2] Forsyth D W. The evolution of the upper mantle beneath mid-ocean ridges[J]. Tectonophysics, 1977, 38(1/2): 89-118.[3] Gaherty J B, Jordan T H, Gee L S. Seismic structure of the upper mantle in a central Pacific corridor[J]. J Geophys Res, 1996, 101(B10): 22 291-22 309.[4] Kawakatsu H, Kumar P, Takei Y, et al. Seismic evidence for sharp lithosphere-asthenosphere boundaries of oceanic plates[J]. Science, 2009, 324: 499-502.[5] Kumar P, Kawakatsu H. Imaging the seismic lithosphere-asthenosphere boundary of the oceanic plate[J]. Geochem Geophys Geosyst, 2011, 12. Q01006, doi:10.1029/2010GC003358.[6] Chapman D S. Thermal gradients in the continental crust[C]//Dawson J B, Carswell D A, Hall J. The Nature of the Lower Continental Crust. Carswell. Geological Society Special Publication, No. 24. Oxford Blackwell Scientific, 1986: 63-70.[7] 臧绍先,刘永刚,宁杰远. 华北地区岩石圈热结构的研究[J]. 地球物理学报,2002, 45(1): 56-66.[8] McKenzie D, Jackson J, Priestley K. Thermal structure of oceanic and continental lithosphere[J]. Earth Planet Sci Lett, 2005, 233: 337-349.[9] An M J, Shi Y L. Lithospheric thickness of the Chinese continent[J]. Phys Earth Planet Int, 2006, 159(3/4):257-266.[10] ArtemievaIy M. The lithosphere: an interdisciplinary approach[M]. New York: Cambridge University Press, 2011.[11] Gaherty J B, Jordan T H. Lehmann discontinuity as the base of an anisotropic layer beneath continents[J]. Science, 1995, 268:1 468-1 471.[12] Debayle E, Kennett B L N. The Australian continental upper mantle: structure and deformation inferred from surface waves[J]. J Geophy Res, 2000, 105(B11): 25 423-25 450.[13] Fischer K M, Ford H A, Abt D L, et al. The lithosphere-asthenosphere boundary[J]. Annu Rev Earth Planet Sci, 2010, 38:551-575. doi:10.1146/annurev-earth-040809-152438.[14] Eaton D W, Darbyshire F, Evans R L, et al. The elusive lithosphere-asthenosphere boundary (LAB) beneath cratons[J]. Lithos, 2009, 109: 1-22.[15] Dragoni M, Pasquale V, Verdoya M, et al. Rheological consequences of the lithospheric thermal structure in the Fennoscandian Shield[J]. Global and Planetary Change, 1993, 8: 113-126.[16] 魏荣强. 鄂尔多斯及其邻区岩石圈三维流变结构的研究 .北京:北京大学,2005.[17] Jones A G. Imaging the continental upper mantle using electromagnetic methods[J]. Lithos, 1999, 48: 57-80.[18] Rudnick L R, Nyblade A A. The thickness and heat production of Archean lithosphere: constraints from xenolith thermobarometry and surface heat flow.[C]//Fei Y, Bertka C M, Mysen B O. Mantle Petrology: Field Observations and High Pressure Experimentation: A Tribute to Francis. R (Joe) Boyd Chem Soc Spec, 1999(The Geochemical Society, Houston, TX, 1999), 6:3-12.[19] Burov E B, Diament M. The effective elastic thickness (Te) of continental lithosphere: What does it really mean?[J] J Geophys Res, 1995, 100(B3): 3 895-3 904.[20] Hirth G, Kohlstedt D L. Water in the oceanic upper mantle: implications for rheology, melt extraction and the evolution of the lithosphere[J]. Earth Planet Sci Lett, 1996, 144(1/2): 93-108.[21] Yuan H Y, Romanowicz B. Lithospheric layering in the North American craton[J]. Nature, 2010, 466:1 063-1 068. doi: 10.1038/nature09332.[22] Artemieva I M, Walter D, Mooney W D. On the relations between cratonic lithosphere thickness, plate motions, and basal drag[J]. Tectonophysics, 2002, 358(1-4): 211-231.[23] Jones M Q. Heat flow in the Witwatersrand basin and environs and its significance for the South African Shield geotherm and lithosphere thickness[J]. J Geophys Res, 1988, 93(B4): 3 243-3 260.[24] Kukkonen I T, Peltonen P. Xenolith-controlled geotherm for the central Fennoscandian Shield: implications for lithosphere-asthenosphere relations[J]. Tectonophysics, 1999, 304(4): 301-315.[25] Russell J K, Dipple G M, Kopylova M G. Heat production and heat flow in the mantle lithosphere, Slave Craton, Canada[J]. Phys Earth Planet Int, 2001, 123(1): 27-44.[26] Li A, Burke K. Upper mantle structure of southern Africa from Rayleigh wave tomography[J]. J Geophys Res, 2006, 111. B10303. doi:10.1029/2006JB004321.[27] Chen C W, Rondenay S, Weertatatne D S, et al. New constraints on the upper mantle structure of the Slave craton from Rayleigh wave inversion[J]. Geophy Res Let, 2007, 34(10), L10301. doi:10.1029/2007GL029535.[28] Bruneton M, Pedersen H A, Farra V, et al. Complex lithospheric structure under the central Baltic Shield from surface wave tomography[J]. J Geophys Res, 2004, 109(B10):B10303. doi:10.1029/2003JB002947.[29] Miensopust M, Jones A G, Garcia X, et al. Lithospheric studies of major Archean cratons and their Proterozoic bounding belts in southern Africa using MT[C]//British Geophysical Association Postgraduate Meeting. Edinburgh, 31 Aug-1 Sep, 2006.[30] Jones A G, Lezeata P, Ferguson I A, et al. The electrical structure of the Slave craton[J]. Lithos, 2003, 71: 505-527.[31] Korja T. How is the European lithosphere imaged by magnetotellurics?[J] Surveys in Geophysics, 2007, 28(2/3): 239-272.[32] Ranalli G. Rheology of the Earth, Chapman & Hall[M]. London, UK, 1995:382.[33] Korenaga J, Karato S. A new analysis of experimental data on olivine rheology[J]. J Geophys Res, 2008, 113(B2):B02403. doi:10.1029/2007JB005100.[34] Karato S, Wu P. Rheology of the upper mantle: a synthesis[J]. Science, 1993, 260: 771-778.[35] Jaupart C, Mareschal J C, Guillou-Frottier L, et al. Heat flow and thickness of the lithosphere in the Canadian Shield[J]. J Geophys Res, 1998, 103(B7): 15 269-15 286.[36] Kirby S H. Rheology of the lithosphere[J]. Rev Geophys Space Phys, 1983, 21(6): 1 458-1 487.[37] Kirby S H, Kronenberg A K. Rheology of the lithosphere: Selected topics[J]. Rev Geophys, 1987, 25(6): 1 219-1 244. |
