Brace W F, Kohlstedt D L. Limits on Lithospheric Stress Iimposed by Labroratory Experiments [J]. J Geophys Res, 1980, 85: 6248-6252.
[2]
Kohlstedt D L, Evans B, Mackwell S J. Strength of the Lithosphere: Constraints Imposed by Laboratory Experiments [J]. J Geophys Res, 1995, 100: 17587-17602.
[3]
Jackson J. Strength of the Continental Lithosphere: Time to Abandon the Jelly Sandwich? [J]. GSA Today, 2002: 4-9.
[4]
Sibson R H. Fault Zone Models, Heat Flow, and Thedepth Distribution of Earthquakes in the Continental Crust of the United States [J]. Bull Seismol Soc Am, 1982, 72: 151-163.
[5]
Chen I-W, Molnar P. Focal Depths of Intracontinental and Intraplate Earthquakes and Their Implications for theThermal and Mechanical Properties of Lithosphere [J]. J Geophys Res, 1983, 88: 4183-4214.
[6]
Zhou Y S, He C R. The Relationship between Low Velocity Layers and Rheology of the Crust in North China and Its Effect on Strong Earthquake [J]. Seismology and Geology, 2002, 24(1): 124-132. (in Chinese).
Zhou Y S, He C R. Rheological Parameters of Orustal Rocks and Crustal Rheology of North China [J]. Seismology and Geology, 2003, 25(1): 109-122. (in Chinese)
Tse S T, Rice J R. Crustal EarthquakeInstability in Relation to the Depth Variation of Frictional Slip Properties [J]. J Geophys Res, 1986, 91: 9452-9472.
[11]
He C R, Ma S L, Huang J G. Influence of Loading Rate Variation on the Stability of Fault Motion [J]. Seismology and Geology, 1998, 20(1): 54-62. (in Chinese)
He C R. Numerical Simulation of Earthquake Nucleation Process and Seismic Precursors on Faults [J]. Earthquake Research in China, 2000, 14(3), 199-212.
[14]
He C R. Interaction between Two Sliders in a System with Rate- and State-Dependent Friction [J]. Science in China (Series D), 2003, 46(Supp): 67-74.
[15]
He C R, Ma S, Huang J. Transition between Stable Sliding and Stick-Slip due to Variation in Slip Rate under Variable Normal Stress Condition [J]. Geophys Res Lett, 1998, 25: 3235-3238.
[16]
He C R, Wong T-F, Beeler N M. Scaling of Stress Drop with Recurrence Interval and Loading Velocity for Laboratory-Derived Fault Strength Relations [J]. J Geophys, Res, 2003, 108(B1): 2037.
[17]
Gu Y, Wong T-F. Effects of Loading Velocity, Stiffness, and Inertia on the Dynamics of a Single Degree of Freedom Spring-Slider System [J]. J Geophys Res, 1991, 96: 21677-21691.
[18]
Boatwright J, Cocco M. Frictional Constraints on Crustal Faulting [J]. J Geophys Res, 1996, 101: 13895-13909.
[19]
Zhou Y S, He C R. Temporal Evolution of Focal Depths of Aftershock Sequence Following Lijiang ms7. 1 Earthquake and the Implication for Rheological Property of the Middle Crust [A]//The 3st International Conference on Continental Earthquakes [C]. Beijing, 2004: 128.
[20]
Scholz C H. The Brittle-Plastic Transition and Depth of Seismic Faulting [J]. Geol Rund, 1988, 77: 319-328.
[21]
Hirth G, Tullis J. The Brittle-Plastic Transition in Experimentally Deformation Quartz Aggregates [J]. J Geophys Res, 1994, 99: 11737-11747.
[22]
Tullis J, Yund R A. Transition from Cataclastic Flow to Dislocation Creep of Feldspar: Mechanisms and Microstructures [J]. Geology, 1987, 15: 606-609.
[23]
Tullis J, Yund R A. The Brittle-Ductile Ttransition in Feldspar Aggregates: An Experimental Study [A]//Fault Mechanics and Transport Properties of Rocks [C]. Academic San Diego, Calif, 1992: 89-117.
[24]
Zhou Y S, Jiang H K, He C R. Experiments of Brittle-Plastic Transition, Modes of Instability of Juyongguan Granite Different T-P Conditions [J]. Earthquake Research in China, 2003, 17(2): 169-182
[25]
Carter N L, Tsenn M C. Flow Properties of Continental Lithosphere [J]. Tectonophysics, 1987, 136: 27-63.
[26]
Gleason G C, Tullis J. A Flow Law for Dislocation Creep of Quartz Aggregates Determined with the Molten Salt Cell [J]. Tectonophysics, 1995, 247: 1-23.
[27]
Zhou Y S, He C R. The Status of Continental Lithosphere Rheology and Experiments on Creep of Rocks at High Temperature and High Pressure [J]. Progress in Geophysical, 2004, 19(2): 246-254. (in Chinese)
Stipp M, Stunitz H. The Eastern Tonale Fault Zone: A "Natural Laboratory" for Crystal Plastic Deformation of Quartz over a Temperature Range from 250 to 700 ℃ [J]. J Struct Geol, 2002, 24: 1861-1884.
[30]
He C R, Zhou Y S, Sang Z N. An Experimental Study on Semi-Brittle and Plastic Rheology of Panzhihua Gabbro [J]. Science in China, Series D, 2003. 46(7): 730-742.
[31]
Zhou Y S, He C R, Song J, et al. An Experiment Study Quartz-Coesite Transition at Differential Stress [J]. Chinese Science Bulletin, 2005, 50(5): 446-451.
[32]
Zhu A L, Xu X W, Zhou Y S, et al. Relocation of Small Earthquakes in Western Sichuan, China and Its Implications for Active Tectonics [J]. Chinese Journal of Geophysis, 2005, 48(3): 692-700.
