Superbrittleness of rocks and earthquake activity
暂无分享,去创建一个
[1] W. Brace,et al. Stick-Slip as a Mechanism for Earthquakes , 1966, Science.
[2] High-Pressure Mechanical Instability in Rocks , 1969, Science.
[3] W. R. Wawersik,et al. Post-failure behavior of a granite and diabase , 1971 .
[4] Arvid M. Johnson,et al. Crack growth and faulting in cylindrical specimens of chelmsford granite , 1972 .
[5] Paul Segall,et al. Mechanics of discontinuous faults , 1980 .
[6] R. Sibson. Fault zone models, heat flow, and the depth distribution of earthquakes in the continental crust of the United States , 1982 .
[7] A. McGarr,et al. SOME APPLICATIONS OF SEISMIC SOURCE MECHANISM STUDIES TO ASSESSING UNDERGROUND HAZARD. , 1984 .
[8] Sia Nemat-Nasser,et al. Compression‐induced microcrack growth in brittle solids: Axial splitting and shear failure , 1985 .
[9] H. Kanamori,et al. Global survey of aftershock area expansion patterns , 1985 .
[10] Chris Marone,et al. The depth of seismic faulting and the upper transition from stable to unstable slip regimes , 1988 .
[11] Stephen H. Hartzell,et al. Aftershock patterns and main shock faulting , 1988 .
[12] C. Scholz,et al. On the formation and growth of faults: an experimental study , 1988 .
[13] A. Aydin,et al. Effect of mechanical interaction on the development of strike-slip faults with echelon patterns , 1990 .
[14] D. Lockner,et al. Quasi-static fault growth and shear fracture energy in granite , 1991, Nature.
[15] G. King,et al. The mechanisms of finite brittle strain , 1992 .
[16] Note on fault-slip motion inferred from a study of micro-cataclastic particles from an underground shear rupture , 1992 .
[17] S. Ruben,et al. Identification of a Naturally Occurring Transforming Variant of the p65 Subunit of NF-KB , 1992, Science.
[18] D. Lockner. The role of acoustic emission in the study of rock fracture , 1993 .
[19] William H. K. Lee,et al. Fine Structure of the Landers Fault Zone: Segmentation and the Rupture Process , 1994, Science.
[20] D. Lockner,et al. Nucleation and growth of faults in brittle rocks , 1994 .
[21] J. Vermilye,et al. Evidence for aseismic deformation in the western Transverse Ranges, southern California: Implications for seismic risk assessment , 1998 .
[22] Z. Reches. Mechanisms of slip nucleation during earthquakes , 1999 .
[23] R. Stein. The role of stress transfer in earthquake occurrence , 1999, Nature.
[24] K. Nishigami. Deep crustal heterogeneity along and around the San Andreas fault system in central California and its relation to the segmentation , 2000 .
[25] O. Nishizawa,et al. Quasi‐static fault growth and cracking in homogeneous brittle rock under triaxial compression using acoustic emission monitoring , 2000 .
[26] Massimo Cocco,et al. Fault interaction by elastic stress changes: New clues from earthquake sequences , 2001 .
[27] Experimental Physics and Rock Mechanics (Results of Laboratory Studies) , 2001 .
[29] Boris Tarasov,et al. The phenomenon of anomalous rock embrittlement , 2005 .
[30] Mark Randolph,et al. Frictionless shear at great depth and other paradoxes of hard rocks , 2008 .
[31] B. Tarasov. Intersonic shear rupture mechanism , 2008 .
[32] A. Aydin,et al. Segmentation along Strike-Slip Faults Revisited , 2009 .
[33] B. Tarasov. Superbrittleness of rocks at high confining pressure , 2010 .