Christie J M, Heard H C, LaMori P N. Experimental deformation of quartz single crystals at 27-30 kb confining pressure and 24 degrees[J]. Geological Society of America Bulletin, 1960,71(12) :1842.
[2]
Turner F J,Griggs D T,Heard H C. Experimental deformation of calcite crystals[J]. Geological Society of America Bulletin,1954,65(9) :883～933.
[3]
Rutter E H. The influence of temperature, strain rate and interstitial water in the experimental deformation of calcite rocks[J].Tectonophysics, 1974,22(3～4) :311～334.
[4]
Kronenberg A K, Tullis J. Flow strengths of quartz aggregates:grain size and pressure effects due to hydrolytic weakening[A].In: Kirby S H, Scholz C H (eds). Chemical effects of water on the strength and deformation of crustal rocks [C]. Journal of Geophysical Research, 1984,B89(6) :4281～4297.
[5]
Keeb H, Wenk H R, Experimental deformation of limestonetexture transitions and comparison of pure and simple shear [J].Terra Cognita, 1988,8(1) :67～68.
[6]
Tullis J. Deformation of granitic rocks: experimental studies and natural example[J]. Reviews in Mineralogy and Geochemistry, 2002,51:51～95.
[7]
Heard H C. Effects of large changes in strain rate in experimental deformation of Yule marble[J]. Journal of Geology, 1963,71:162～195.
[8]
Turner F J, Griggs D T, Heard H C, et al. Plastic deformation of dolomite rock at 38℃[J]. American Journal of Science,1954,252: 477～488.
[9]
Shimada M, Liu J. Temperature dependence of strength of rocks under high confining pressure: micromechanism and implications[M]. Disaster Prevention Research Institute Annuals, 2000,43(B-1) :75～84.
[10]
Shimada M. Lithosphere strength inferred from fracture strength of rocks at high confining pressures and temperatures[J]. Tectonophysics, 1993,217(1-2) :55～64.
[11]
Bozkurt E, Park R G. Microstructures of deformed grains in the Augen gneisses of southern Menderes Massif (western Turkey) and their tectonic significance[J]. Geologische Rundschau, 1997,86(1) :103～119.
[12]
Venera Z, Schulmann K, Kroener A. Intrusion within a transtensional tectonic domain, the Cista Granodiorite (Bohemian Massif): structure and rheological modeling[J]. Journal of Structural Geology, 2000,22(10):1437～1454.
[13]
Kennedy L A, White J C. Low-temperature recrystallization in calcite: Mechanisms and consequences[J]. Geology, 2001,29:1027～1030.
[14]
Liu Junlai, Jens W, Klaus W. Fluid-enhanced low temperature plasticity of calcite rocks: microstructures and mechanisms[J]. Geology, 2002,30:787～790.
[15]
Brown C D, Phillips R J. Crust-mantle decoupling by flexure of continental lithosphere[J]. Journal of Geophysical Research, B,2000,105(6): 13221～13237.
[16]
Coleman R G, Wang X. Ultrahigh pressure metamorphism[J].Cambridge Univ. Press, 1995.356～390.
[17]
Paterson M S. Problems in the extrapolation of laboratory rheological data[J]. Tectonophysics, 1987,133(1～2) :33～43.
[18]
Van der Pluijm B A, Hall C M, Vrolijk P J, et al. The dating of shallow faults in the Earth\'s crust[J]. Nature, 2001,412:172～175.
[19]
Muller W, Aerden D, Halliday A. Isotopic dating of strain fringe increments: Duration and rates of deformation in shear zones[J]. Science, 2000,288(23) :2195～2198.
[20]
Foster D A, Raza A. Low-temperature thermochronological record of exhumation of the Bitterroot metamorphic core complex, northern Cordilleran Orogen[J]. Tectonophysics, 2002,349:23～36.
[21]
Foster D A, John B E. Quantifying tectonic exhumation in an extensional orogen with thermochronology: examples from the southern Basin and Range Province [A]. In: Ring U, et al (eds). Exhumation processes: Normal faulting, ductile flow,and erosion[M]. Geological Society of London, Special Publication, 1999,154:356～378.
[22]
Tarduno J A, Duncan R A, Scholl D W, et al. The Emperor seamounts: southward motion of the Hawaiian hotspot plume in Earth\'s mantle[J]. Science, 2003,301:1064～1069.
[23]
htrp://www. outlook.moaa.gov/98hurricanes.
[24]
Bascou J, Barruol G, Vauchez A, et al. EBSD-measured lattice-preferred orientations and seismic properties of eclogites[J].Tectonophysics, 2001,342 (1～2): 61～80.
[25]
Lloyd G E. Grain boundary contact effects during faulting of quartzite: an SEM/EBSD analysis[J]. Journal of Structural Geology, 2000,22(11～12): 1675～1693.
[26]
Tackley P J. Mantle convection and plate tectonics: toward an integrated physical and chemical theory[J]. Science, 2000,288:2002～2007.
[27]
Solomatov V S, Moresi L N. Plate tectonics and mantle convection with ductile/brittle rheology[J]. Eos, Transactions, American Geophysical Union, 1997,78(17) :322.
Vauchez A, Tommasi A, Barruol G. Rheological heterogeneity,mechanical anisotropy and deformation of the continental lithosphere[J]. Tectonophysics, 1998,296:61～86.
[30]
Storti F, Holdsworth R E, Salvini F. Intraplate strike-slip deformation belts[A]. In: Storti F, Holdsworth R E, Salvini F(eds). Intraplate strike-slip deformation belts[C]. Geological Society Special Publications, 2003,210:1～14.
[31]
Carter N L, Tsenn M C. Flow properties of continental lithosphere[J]. Tectonophysics, 1987,136:27～63.
[32]
Kenner S J. Localized intraplate weak zones, sources of stress and the spatial distributon of seismic slip[A]. In: Abstracts with Programs[C]. Geological Society of America, 2002,34(6):78.
[33]
Liu J, Xu C, Song C, et al. Using repeated precise GPS campaigns for research of present-day crustal movement and strain in the Qinghai-Tibet Plateau[J]. Chinese Science Bulletin, 2001,46(8) :694～698.
[34]
Li B, Niu Z, Duan F. Preliminary analysis for the roles of crustal low-velocity and high-conductivity body in process of strong earthquake preparation[J]. Acta Seismologica Sinica, 2000,13(2): 151～158.
[35]
Maggi A, Jackson J A, McKenzie D, et al. Earthquake focal depths, effective elastic thickness, and the strength of the continental lithosphere[J]. Geology, 2000,28 (6): 495～498.
[36]
Peter Bird. Lithosphere dynamics and continental deformation[J].Reviews of Geophysics, 1995, (suppl.):379～383.
[37]
Shimada M, Cho A. Two types of brittle fracture of silicate rocks under confining pressure and their implications in the earth\'s crust[J]. Tectonophysics, 1990,175(1～3):221～235.
[38]
Sibson R H. Fault rocks and fault mechanisms[J]. Joumal of the Geological Society of London, 1977,133:191～213.
[39]
Sibson R H. Continental fault structure and the shallow earthquake source[J]. J. Geol. Soc. Lond., 1983,140:741～767.
[40]
Rutter E H. The influence of temperature, strain rate and interstitial water in the experimental deformation of calcite rocks[J].Tectonophysics, 1974,22:311～334.
[41]
Scholz C H. The mechanics of earthquakes and faulting[M].Cambridge: Cambridge University Press,1990.439.
[42]
Kawamoto E, Shimamoto T. Mechanical behavior of halite and calcite shear zones from brittle to fully plastic deformation and a revised fault model[A]. In: Zheng Yadong, Davis G A, Yin An (eds). Proc. 30th Int. Geol. Congr[C]. 1996,14:89～105.
[43]
Babuska V, Plomerova J, Sileny J. Models of seismic anisotropy in the deep continental lithosphere[J]. Physics of the Earth and Planetary Interiors, 1993,78(3～4) :167～191.
[44]
Jackson J. Faulting, flow, and the strength of the continental lithosphere[J]. International Geology Review, 2002,44(1) :39～61.
[45]
Zhang Z, Zhu X. Potential applications of nano-scale science and technology in geosciences and experimental studies of nanometer-sized gold adsorption on minerals and rocks[J]. Chinese Journal of Geochemistry, 1997,16(2): 133～138.
[46]
赵新宇.纳米世纪[M].广州:广州出版社,2001.228.
[47]
Krinsley D, Dorn R, Tovey N K. Nanometer-scale layering in rock varnish: implications for genesis and paleoenvironmental interpretation[J]. Journal of Geology, 1995,103(1): 106～113.
[48]
Riller U, Schwerdtner W M, Robin P Y F. Low-temperature deformation mechanisms at a lithotectonic interface near the Sudbury Basin, eastern Penokean Orogen, Canada[J]. Tectonophysics, 1998,287 (1～4): 59～75.
[49]
Kennedy L A, Logan J M. Microstructures of cataclasites in a limestone-on-shale thrust fault: Implications for low-tempera ture recrystallization of calcite[J]. Tectonophysics, 1998,284:167～186.
