何昌荣,周永胜,桑祖南.2002.四川攀枝花辉长岩半脆性-塑性流变的实验研究[J].中国科学(D辑),32(9): 717-726.
HE Chang-rong,ZHOU Yong-sheng,SANG Zu-nan.2002.The experimental study of semibrittle-plastic rheology of Panzhihua gabbro in Sichuan Province[J].Science in China(Ser D),32(9): 717-726(in Chinese).
刘力强,马胜利,马瑾,等.1999.岩石构造对声发射统计特征的影响[J].地震地质,21(4): 377-386.
LIU LI-qiang,MA Sheng-li,MA Jin,et al.1999.Effect of rock structure on statistic characteristics of acoustic emission[J].Seismology and Geology, 21(4): 377-386(in Chinese).
马胜利,Lockner D,Moore D,等.1997.水热作用条件下蛇纹石断层泥的摩擦强度和速度依赖性及其地震地质意义[J].地震地质,19(2): 171-178.
MA Sheng-li,Lockner D,Moore D,et al.1997.Frictional strength and velocity-dependence of serpentine gouges under hydrothermal conditions and their seismogelogical implications[J].Seismology and Geology,19(2): 171-178(in Chinese).
缪阿丽,马胜利,侯林峰,等.2012.岩盐断层带摩擦滑动的速度依赖性转换及其地震学意义[J].地球物理学报,(出版中).
MIAO A-li,MA Sheng-li,HOU Lin-feng,et al.2012.Velocity-dependence transition of friction for halite gouge and its significance in seismology[J].Chinese J Geophys,(in press).
Bartlett W L,Friedman M,Logan J M.1981.Experimental folding and faulting of rocks under confining pressure[J].Tectonophysics,79: 255-277.
Blacic J D,Christle J M.1984.Plasticity and hydrolytic weakening of quartz single crystals[J].J Geophys Res,89(B6): 4223-4239.
Blanpied M L,Lockner D A,Byerlee J D.1995.Frictional slip of granite at hydrothermal conditions[J].J Geophys Res,100(B7): 13045-13064.
Bos B,Peach C J,Spiers C J.2000.Frictional-viscous flow of simulated fault gouge caused by the combined effects of phyllosilicates and pressure solution[J].Tectonophysics,327: 173-194.
Bos B,Spiers C J.2001.Experimental investigation into the microstructural and mechanical evolution of phyllosilicate-bearing fault rock under conditions favouring pressure solution[J].Journal of Structural Geology,23: 1187-1202.
Bos B,Spiers C J.2002.Frictional-viscous flow of phyllosilicate-bearing fault rock: Microphysical model and implications for crustal strength profiles[J].J Geophys Res,107(B2):10.102 9/2001JB000301.
Boutareaud S,Fabbri O,Calugaru D, et al.2008.Clay-clast aggregates: A new textural evidence for seismic fault sliding?[J].Geophys Res Lett,35,L05302.doi: 10.1029/2007GL032554.
Byerlee J D.1967.Frictional characteristics of granite under high confining pressure[J].J Geophys Res,72: 3639-48.
Byerlee J D.1978.Friction of rocks[J].Pure Appl Geophys,116: 615-629.
Collettini C,Niemeijer A,Viti C,et al.2009.Fault zone fabric and fault weakness[J].Nature,462: 907-910.doi: 10.103 8/nature08585.
Dieterich J H.1979.Modelling of rock friction: 1.Experimental results and constitutive equations[J]. J Geophys Res,84: 2161-2168.
Dieterich J H,Conrad G.1984.Effect of humidity on time- and velocity-dependent friction in rocks[J].J Geophys Res,89: 4196-202.
Di Toro G,Hirose T,Nielsen S,et al.2006.Natural and experimental evidence of melt lubrication of faults during earthquakes[J].Science,311: 647-649.
Hansen F D,Carter N L.1983.Semibrittle creep of dry and wet Westly granite at 1000MPa .U S 24th Symp on Rock Mechanics.Texas A & M Univ,College Station,Tes,429-447.
Holdsworth R E.2004.Weak faults-rotten cores[J].Science,303: 181-182.
Imber J,Holdsworth R E,Butler C A,et al.2001.A reappraisal of the Sibson-Scholz fault zone model: The nature of the frictional to viscous("brittle-ductile")transition along a long-lived,crustal-scale fault,Outer Hebrides,Scotland[J].Tectonics,20(5): 601-624.
Moore D E,Lockner D A.2008.Talc friction in the temperature range 25~400℃ relevance for fault-zone weakening[J].Tectonophysics,449: 120-132.
Moore D E,Lockner D A,Ma Shengli,et al.1996.Strength of chrysotile-serpentinite gouge under hydrothermal conditions: Can it explain a weak San Andreas Fault?[J].Geology,24(11): 1041-1044.
Moore D E,Lockner D A,Ma Shengli,et al.1997.Strengths of serpentinite gouges at elevated temperatures[J].J Geophys Res,102: 14,787-14,801.
Moore D E,Lockner D A,Tanaka H,et al.2004.The coefficient of friction of chrysotile gouge at seismogenic depths .In: Ernst,W G(ed) Serpentine and Serpentinites: Mineralogy,Petrology,Geochemistry,Ecology,Geophysics,and Tectonics.Geol Soc Am Internat Book Ser,l(8): 525-538.
Moore D E,Rymer M.2007.Talc-bearing serpentinites and the creeping section of the San Andreas Fault[J].Nature,448: 795-797.doi: 10.1038/nature06064.
Niemeijer A R,Spiers C J.2006.Velocity dependence of strength and healing behaviour in simulated phyllosilicate-bearing fault gouge[J].Tectonophysics,427: 231-253.
Reinen L A,Weeks J D,Tullis T E.1991.The frictional behavior of serpentinite: Implications for aseismic creep on shallow crustal faults[J].Geophys Res Lett,18: 1921-1924.
Reinen L A,Weeks J D,Tullis T E.1994.The frictional behavior of lizardite and antigorite serpentinites: Experiments,constitutive models,and implications for natural faults[J].Pure Appl Geophys,143: 317-358.
Ruina A L.1983.Slip instability and state variable friction[J].J Geophys Res,88: 10359-10370.
Scholz C H.2002.The Mechanics of Earthquakes and Faulting(2nd Edition)[M].Cambridge University Press.1-508.
Scruggs V J,Tullis T E.1998.Correlation between velocity dependence of friction and strain localization in large displacement experiments on feldspar,muscovite and biotite gouge[J].Tectonophysics,295: 15-40.
Van Diggelen E W E,De Bresser J H P,Peach C J,et al.2009.High shear strain behavior of synthetic muscovite fault gouges under hydrothermal conditions[J].J Struct Geol,32(11): 1685-1700.doi: 10.1016/j.jsg.2009.08.020.
Wibberley C A J,Shimamoto T.2005.Earthquake slip weakening and asperities explained by thermal pressurization[J].Nature,436: 689-692.
Wibberley C A J,Kurz W,Imber J,et al.2008.The internal structure of fault zones: Implications for mechanical and fluid-flow properties[M].Geological Society of London,Special Publication,299: 151-173.
Wilks K R,Carter N L.1990.Rheology of some continental lower crustal rocks[J].Tectonophysics,182: 57-77.
Wintsch R P,Christoffersen R,Kronenberg A K.1995.Fluid-rock reaction weakening of fault zones[J].J Geophys Res,100: 13021-13032. |