Abe, Y., and Kato, N. 2013. Complex earthquake cycle simulations using a two-degree-of-freedom spring-block model with a rate- and state-friction law. Pure Appl. Geophys 170(5): 745–765, doi: 10.1007/s00024-011–0450-8.Google Scholar

Aben, F. M., Doan, M. L., Mitchell, T. M., et al. 2016. Dynamic fracturing by successive coseismic loadings leads to pulverization in active fault zones. J. Geophys. Res.-Solid Earth 121(4): 2338–2360, doi: 10.1002/2015jb012542.CrossRefGoogle Scholar

Abercrombie, R. E. 1995. Earthquake source scaling relationships from −1 to 5 M(L) using seismograms recorded at 2.5-km depth. J. Geophys. Res.-Solid Earth 100: 24015–24036.Google Scholar

Abercrombie, R. E., Agnew, D. C., and Wyatt, F. K. 1995. Testing a model of earthquake nucleation. Bull. Seismol. Soc. Amer. 85: 1873–1878.Google Scholar

Abercrombie, R. E., and Ekström, G. 2001. Earthquake slip on oceanic transform faults. Nature 410: 74–76.CrossRefGoogle ScholarPubMed

Abercrombie, R. E., and Ekström, G. 2003. A reassessment of the rupture characteristics of oceanic transform earthquakes. J. Geophys. Res.-Solid Earth 108(B5): doi: 10.1029/2001jb000814.Google Scholar

Abercrombie, R. E., and Mori, J. 1996. Occurrence patterns of foreshocks to large earthquakes in the western United States. Nature 381(6580): 303–307.Google Scholar

Abercrombie, R. E., and Rice, J. R. 2005. Can observations of earthquake scaling constrain slip weakening? Geophys. J. Int. 162: 406–424,Google Scholar

Abercrombie, R. E., Antolik, M., Felzer, K., and Ekström, G. 2001. The 1994 Java tsunami earthquake: Slip over a subduction seamount. J. Geophys. Res. 106: 6595–6608.CrossRefGoogle Scholar

Abers, G. A. 1991. Possible seismogenic shallow-dipping normal faults in the Woodlark-Dentrecasteaux Extensional Province, Papua-New-Guinea. Geology 19: 1205–1208.2.3.CO;2>CrossRefGoogle Scholar

Abers, G. A. 2005. Seismic low-velocity layer at the top of subducting slabs: Observations, predictions, and systematics. Phys. Earth Planet. Int. 149(1–2): 7–29, doi: 10.1016/j.pepi.2004.10.002.CrossRefGoogle Scholar

Acebron, J. A., Bonilla, L. L., Vincente, J. P., Ritort, F., and Spigler, R. 2005. The Kuramoto model: A simple paradigm for synchronization phenomena. Rev. Mod. Phys. 77: 137–185.Google Scholar

Achenbach, J. D. 1973. Dynamic effects in brittle fracture. In Mechanics Today, New York: Pergamon, pp. 1–57.Google Scholar

Ackermann, R. V., and Schlische, R. W. 1997. Anticlustering of small normal faults around larger faults. Geology 25: 1127–1130.Google Scholar

Ackermann, R. V., Schlische, R. W., and Withjack, M. O. 2001. The geometric and statistical evolution of normal fault systems: An experimental study of the effects of mechanical layer thickness on scaling laws. J. Struct. Geol. 23(11): 1803–1819.Google Scholar

Adams, F. D. 1938. The Growth and Development of the Geological Sciences. Baltimore: Williams and Wilkins.Google Scholar

Adams, J., Wetmiller, R. J., Hasegawa, H. S., and Drysdale, J. 1991. The 1st surface faulting from a historical intraplate earthquake in North-America. Nature 352: 617–619.Google Scholar

Aderhold, K., and Abercrombie, R. E. 2016a. The 2015 M-w 7.1 earthquake on the Charlie-Gibbs transform fault: Repeating earthquakes and multimodal slip on a slow oceanic transform. Geophys. Res. Lett. 43(12): 6119–6128, doi: 10.1002/2016gl068802.Google Scholar

Aderhold, K., and Abercrombie, R. E. 2016b. Seismotectonics of a diffuse plate boundary: Observations off the Sumatra-Andaman trench. J. Geophys. Res.-Solid Earth 121(5): 3462–3478, doi: 10.1002/2015jb012721.Google Scholar

Aggarwal, Y. P., Sykes, L. R., Simpson, D. W., and Richards, P. G. 1973. Spatial and temporal variations of tJtp and in P wave residuals at Blue Mountain Lake, New York: Application to earthquake prediction. J. Geophys. Res. 80: 718–732.Google Scholar

Aguiar, A. C., Melbourne, T. I., and Scrivner, C. W. 2009. Moment release rate of Cascadia tremor constrained by GPS. J. Geophys. Res.-Solid Earth 114, doi: 10.1029/2008jb005909.Google Scholar

Aharonov, E., and Scholz, C. H. 2018a. A physics-based friction constitutive law: Steady state friction, J. Geophys. Res. 123: 1591–1614, doi: 10.1002/2016JB013829.Google Scholar

Aharonov, E., and Scholz, C. H. 2018b. The brittle-ductile transition predicted by a physics-based friction law, J. Geophys. Res. subm.Google Scholar

Aki, K. 1966. Generation and propagation of G waves from the Niigata earthquake of June 16, 1964, 2, Estimation of earthquake moment, released energy, and stress-strain drop from G wave spectrum. Bull. Earthquake Res. Inst., Univ. Tokyo 44: 73–88.Google Scholar

Aki, K. 1967. Scaling law of seismic spectrum. J. Geophys. Res. 72: 1217–1231.CrossRefGoogle Scholar

Aki, K. 1979. Characterization of barriers on an earthquake fault. J. Geophys. Res. 84: 6140–6148.Google Scholar

Aki, K. 1981. A probabilistic synthesis of precursory phenomena. In Earthquake Prediction, an International Review. Ewing, M.; Ser. 4, eds. Simpson, D. and Richards, P.. Washington, DC: American Geophysical Union, pp. 566–574.Google Scholar

Aki, K. 1984. Asperities, barriers and characteristics of earthquakes. J. Geophys. Res. 89: 5867–5872.Google Scholar

Aki, K. 1985. Theory of earthquake prediction with special reference to monitoring of the quality factor of lithosphere by coda method. Earthquake Pred. Res. 3: 219–230.Google Scholar

Aki, K. 1987. Magnitude frequency relation for small earthquakes: A clue for the origin of fmax of large earthquakes. J. Geophys. Res. 92: 1349–1355.Google Scholar

Aki, K., and Richards, P. 2002. Quantitative Seismology, 2nd edn., University Science Books.Google Scholar

Alessio, G., et al. 2010. Evidence for surface rupture associated with the Mw 6.3 L’Aquila earthquake sequence of April 2009 (central Italy). Terra Nova 22(1): 43–51, doi: 10.1111/j.1365–3121.2009.00915.x.Google Scholar

Allegre, C. J., Le Mouel, J. L., and Provost, A. 1982. Scaling rules in rock fracture and possible implications for earthquake prediction. Nature 297: 47–49.CrossRefGoogle Scholar

Allen, C. R. 1968. The tectonic environment of seismically active and inactive areas along the San Andreas fault system. In Proc. Conf. on Geological Problems of the San Andreas Fault System, ed. Kovach, R., Stanford Univ. Publ Geol. Sci., pp. 70–82.Google Scholar

Allen, C. R. 1969. Active Faulting in Northern Turkey. Contr. No. 1577. Div. Geol. Sci. Calif. Inst. Tech. 32.Google Scholar

Allen, C. R., Wyss, M., Brune, J., Grantz, A., and Wallace, R. 1972. Displacements on the Imperial, Superstition Hills, and San Andreas faults triggered by the Borrego Mountain earthquake: The Borrego Mountain Earthquake of April 9, 1968. US Geol Surv. Prof. Paper 787: 87–104.Google Scholar

Allen, R. M., and Kanamori, H. 2003. The potential for earthquake early warning in southern California. Science 300(5620): 786–789, doi: 10.1126/science.1080912.Google Scholar

Allen, R. M., Gasparini, P. Kamigaichi, O., and Böse, M. 2009. The status of earthquake early warning around the world: An introductory overview. Seismol. Res. Lett. 80(5): 682–693.Google Scholar

Allmann, B. P., and Shearer, P. M. 2009. Global variations of stress drop for moderate to large earthquakes. J. Geophys. Res.-Solid Earth 114(B1): doi: 10.1029/2008jb005821.Google Scholar

Alt, R. C., and Zoback, M. D. 2017. In Situ Stress and Active Faulting in Oklahoma. Bull. Seismol. Soc. Am. 107(1): 216–228, doi: 10.1785/0120160156.Google Scholar

Amato, A., Azzara, R., Chiarabba, C., et al. 1998. The 1997 Unbria-Marche, Italy, earthquake sequence: A first look at the mainshocks and aftershocks. Geophys. Res. Lett. 25: 2861–2864.Google Scholar

Ambraseys, N., and Finkel, C. 1988. The Anatolian earthquake of 17 August 1668. In Historic Seismograms and Earthquakes of the World, eds. Lee, H. M. W. H. K., and Shimazaki, K., Academic, San Diego, Calif., pp. 173–180.Google Scholar

Ambrayseys, N. H. 1970. Some characteristic features of the Anatolian fault zone. Tectonophysics 9: 143–165.Google Scholar

Ambrayseys, N. H. 1975. Studies of historical seismicity and tectonics. In Geodynamics Today, A Review of the Earth’s Dynamic Processes, London: The Royal Society, pp. 7–16.Google Scholar

Amelung, F., and King, G. C. P. 1997. Earthquake scaling laws for creeping and non-creeping faults. Geophys. Res. Lett. 24: 507–510.CrossRefGoogle Scholar

Amitrano, D. 2003. Brittle-ductile transition and associated seismicity: Experimental and numerical studies and relationship with the b value. J. Geophys. Res. 108(B1): 2044, doi: 10.1029/2001JB000680.Google Scholar

Amitrano, D., and Helmstetter, A. 2006. Brittle creep, damage, and time to failure in rocks. J. Geophys. Res.-Solid Earth 111 (B11): 1–17, doi: 10.1029/2005jb004252.Google Scholar

Ammon, C. J., Ji, C., Thio, H.-K., Robinson, D., Ni, S., Hjorleifsdottir, V., Kanamori, H., Lay, T., Das, S.,and Helmberger, D. 2005. Rupture process of the 2004 Sumatra-Andaman earthquake. Science 308(5725): 1133–1139.Google Scholar

Ammon, C. J., Kanamori, H., and Lay, T. 2008. A great earthquake doublet and seismic stress transfer cycle in the central Kuril islands. Nature 451(7178): 561–564, doi: 10.1038/nature06521.Google Scholar

Ammon, C. J., Kanamori, H., Lay, T., and Velasco, A. A. 2006. The 17 July 2006 Java tsunami earthquake. Geophys. Res. Lett. 33(24): L24308.Google Scholar

Ampuero, J. P., and Ben-Zion, Y. 2008. Cracks, pulses and macroscopic asymmetry of dynamic rupture on a bimaterial interface with velocity-weakening friction. Geophys. J. Int. 173(2): 674–692, doi: 10.1111/j.1365-246X.2008.03736.x.Google Scholar

Ampuero, J.-P., and Rubin, A. M. 2008. Earthquake nucleation on rate and state faults: Aging and slip laws. J. Geophys. Res. 113, doi: 10.1029/2007JB005082.Google Scholar

Anandakrishnan, S., Voigt, D. E., Alley, R. B. and King, M. A. 2003. Ice stream D flow speed is strongly modulated by the tide beneath the Ross Ice Shelf. Geophys. Res. Lett. 30(7): 1361, doi: 10.1029/2002gl016329.CrossRefGoogle Scholar

Anderlini, L., Serpelloni, E., and Belardinelli, M. E. 2016. Creep and locking of a low-angle normal fault: Insights from the Altotiberina fault in the Northern Apennines (Italy). Geophys. Res. Lett. 43(9): 4321–4329, doi: 10.1002/2016gl068604.Google Scholar

Anders, M. H., and Schlische, R. W. 1994. Overlapping faults, intrabasin highs, and the growth of normal faults. J. Geol. 102(2): 165–180.CrossRefGoogle Scholar

Anders, M. H., and Wiltschko, D. V. 1994. Microfracturing, paleostress and the growth of faults. J. Struct. Geol. 16: 795–815.Google Scholar

Anders, M. H., Laubach, S. E., and Scholz, C. H. 2014. Microfractures: A review. J. Struct. Geol. 69: 377–394, doi: 10.1016/j.jsg.2014.05.011.Google Scholar

Anders, M. H., Spiegelman, M., Rodgers, D. W., and Hagstrum, J. T. 1993. The growth of fault-bounded tilt blocks. Tectonics 12(6): 1451–1459.Google Scholar

Anderson, E. M. 1905. The dynamics of faulting. Trans. Edinburgh Geol. Soc. 8: 387–340.Google Scholar

Anderson, E. M. 1936. The dynamics of the formation of cone-sheets, ring-dykes, and cauldron-subsidences. Proc. Roy. Soc. Edinburgh 56: 128–125.Google Scholar

Anderson, E. M. 1951. The Dynamics of Faulting. Edinburgh: Oliver and Boyd.Google Scholar

Anderson, J. G., and Bodin, P. 1987. Earthquake recurrence models and historical seismicity in the Mexicali-Imperial Valley. Bull. Seismol. Soc. Am. 77: 562–578.Google Scholar

Anderson, J. G., Brune, J. N., Louie, J. N., Zeng, Y., Savage, M., Yu, G., Chen, Q., and dePolo, D. 1994. Seismicity in the western Great Basin apparently triggered by the Landers, California earthquake, 28 June, 1992. Bull. Seismol. Soc. Amer. 84: 863–891.Google Scholar

Anderson, J. G., Wesnousky, S. G., and Stirling, M. W. 1996. Earthquake size as a function of fault slip rate. Bull. Seismol. Soc. Am. 86(3): 683–690.CrossRefGoogle Scholar

Anderson, J. L., Osborne, R., and Palmer, D. 1983. Cataclastic rocks of the San Gabriel fault zone and expression of deformation at deeper crustal levels in the San Andreas fault zone. Tectonophysics 98: 209–251.Google Scholar

Anderson, O. L., and Grew, P. C. 1977. Stress-corrosion theory of crack-propagation with applications to geophysics. Rev. Geophys. 15(1): 77–104, doi: 10.1029/RG015i001p00077.CrossRefGoogle Scholar

Anderson, R. N., Langseth, M. G., and Sclater, J. G. 1977. The mechanisms of heat transfer through the floor of the Indian Ocean. J. Geophys. Res. 82: 3391–3409.Google Scholar

Ando, M. 1974. Seismotectonics of the 1923 Kanto earthquake. J. Phys. Earth 22: 263–277.Google Scholar

Ando, M. 1975. Source mechanisms and tectonic significance of historical earthquakes along the Nankai trough. Tectonophysics 27: 119–140.Google Scholar

Ando, R., and Imanishi, K. 2011. Possibility of M-w 9.0 mainshock triggered by diffusional propagation of after-slip from M-w 7.3 foreshock. Earth Planets and Space, 63(7): 767–771, doi: 10.5047/eps.2011.05.016.Google Scholar

Ando, R., Nakata, R., and Hori, T. 2010. A slip pulse model with fault heterogeneity for low-frequency earthquakes and tremor along plate interfaces. Geophys. Res. Lett. 37, doi: 10.1029/2010gl043056.Google Scholar

Andrews, D. 1976a. Rupture propagation with finite stress in antiplane strain. J. Geophys. Res. 81: 3575–3582.CrossRefGoogle Scholar

Andrews, D. 1976b. Rupture velocity of plane strain shear cracks. J. Geophys. Res. 81: 5679–5687.Google Scholar

Andrews, D. 1980. A stochastic fault model, static case. J. Geophys. Res. 85: 3867–3887.CrossRefGoogle Scholar

Andrews, D. 1985. Dynamic plane strain shear rupture with a slip-weakening friction law calculated by a boundary integral method. Bull. Seismol. Soc. Am. 75: 1–21.Google Scholar

Andrews, D. J. 2005. Rupture dynamics with energy loss outside the slip zone, J. Geophys. Res. 110: 1–14, doi: 10.1029/2004JB003191Google Scholar

Andrews, D. J., and Ben-Zion, Y. 1997. Wrinkle-like slip pulse on a fault between different materials. J. Geophys. Res.-Solid Earth 102: 553–571.Google Scholar

Andrews, D. J., and Harris, R. A. 2005. The wrinkle-like slip pulse is not important in earthquake dynamics, Geophys. Res. Lett. 32: L23303, doi: 10.1029/2005GL023996.Google Scholar

Angellier, J. 1984. Tectonic analysis of fault slip data sets. J. Geophys. Res. 89: 5835–5848.CrossRefGoogle Scholar

Antolik, M., Abercrombie, R. E., Pan, J., and Ekström, G. 2006. Rupture characteristics of the 2003 Mw 7.6 mid‐Indian Ocean earthquake: Implications for seismic properties of young oceanic lithosphere. J. Geophys. Res.-Solid Earth 111(B4).Google Scholar

Antolik, M., Dreger, D., and Romanowicz, B. 1999. Rupture processes of large deep-focus earthquakes from inversion of moment rate functions. J. Geophys. Res.-Solid Earth 104(B1): 863–894, doi: 10.1029/1998jb900042.Google Scholar

Antonellini, M. A., Aydin, A., and Pollard, D. D. 1994. Microstructure of deformation bands in porous sandstone at Arches National Park, Utah. J. Struct. Geol. 16(7): 941–959, doi: 10.1016/0191–8141(94)90077–9.Google Scholar

Aoki, Y., and Scholz, C. H. 2003. Interseismic deformation at the Nankai subduction zone and the Median Tectonic Line, southwest Japan. J. Geophys. Res.-Solid Earth 108(B10).Google Scholar

Archard, J. F. 1953. Contact and rubbing of flat surfaces. J. App. Phy. 24: 981–988.Google Scholar

Archard, J. F. 1957. Elastic deformation and the laws of friction. Proc. R. Soc. London Ser. A 243: 190–205.Google Scholar

Arnadottir, T., and Segal, P. 1994. The 1989 Loma-Prieta earthquake imaged from inversion of geodetic data. J. Geophys. Res.-Solid Earth 99: 21835–21855.Google Scholar

Asano, Y., Saito, T., Ito, Y., Shiomi, K., Hirose, H., Matsumoto, T., Aoi, S., Hori, S., and Sekiguchi, S. 2011. Spatial distribution and focal mechanisms of aftershocks of the 2011 off the Pacific coast of Tohoku Earthquake. Earth Planets and Space, 63(7): 669–673, doi: 10.5047/eps.2011.06.016.Google Scholar

Ashby, M. F., and Sammis, C. G. 1990. The damage mechanics of brittle solids in compression. Pure Appl. Geophys. 133(3): 489–521, doi: 10.1007/bf00878002.Google Scholar

Astiz, L., and Kanamori, H. 1986. Interplate coupling and temporal variation of mechanisms of intermediate-depth earthquakes in Chile. Bull. Seismol. Soc. Am. 76(6): 1614–1622.Google Scholar

Atkinson, B. K. 1980. Stress corrosion and the rate-dependent tensile failure of a fine-grained quartz rock. TTectonophysics 65: 281–290.Google Scholar

Atkinson, B. K. 1984. Subcritical crack growth in geological materials. J. Geophys. Res. 89: 4077–4114.Google Scholar

Atkinson, B. K. 1987. Introduction to fracture mechanics and its geophysical applications. In Fracture Mechanics of Rock, ed. Atkinson, B. K.. London: Academic Press, pp. 1–26.Google Scholar

Atkinson, B. K., and Meredith, P. G. 1987. Experimental fracture mechanics data for rocks and minerals. In Fracture Mechanics of Rock, ed. Atkinson, B. K., Academic Press, London, pp. 477–525.Google Scholar

Atwater, B. F. 1990. Evidence for great Holocene earthquakes along the outer coast of Washington State. Science 236: 942–944.Google Scholar

Atwater, T. 1970. Implications of plate tectonics for the Cenozoic tectonic evolution of western North America. Geol. Soc. Am. Bull. 81: 3513–3536.Google Scholar

Audet, P., Bistock, M. G., Boyarko, D. C., Brudzinski, M. R., and Allen, R. M. 2010. Slab morphology in the Cascadia forearc and its relation to episodic tremor and slip. J. Geophys. Res. 115, b00A16: doi: 10.1029/2008JB006053.Google Scholar

Audet, P., Bostock, M. G., Christensen, N. I., and Peacock, S. M. 2009. Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing. Nature 457(7225): 76–78, doi: 10.1038/nature07650.Google Scholar

Auzende, J. M., Bideau, D., Bonatti, E., et al. 1989. Direct observation of a section through slow-spreading oceanic-crust. Nature 337: 726–729.Google Scholar

Aviles, C. A., Scholz, C. H., and Boatwright, J. 1987. Fractal analyis applied to characteristic segments of the San Andreas fault. J. Geophys. Res.-Solid Earth and Planets 92(B1): 331–344, doi: 10.1029/JB092iB01p00331.Google Scholar

Avouac, J. P. 2015. From geodetic imaging of seismic and aseismic fault slip to dynamic modeling of the seismic cycle. In Ann. Rev. Earth Planet. Sci, Vol 43, eds. Jeanloz, R. and Freeman, K. H., pp. 233–271, doi: 10.1146/annurev-earth-060614–105302.Google Scholar

Axen, G. J. 1992. Pore pressure, stress increase, and fault weakening in low-angle normal faulting. J. Geophys. Res.-Solid Earth 97: 8979–8991.Google Scholar

Aydin, A. 1978. Small faults formed as deformation bands in sandstone. Pure Appl. Geophys. 116(4–5): 913–930, doi: 10.1007/bf00876546.Google Scholar

Aydin, A., and Johnson, A. M. 1978. Development of faults as zones of deformation bands and as slip surfaces in sandstone. Adv. Appl. Mech. 116: 922–929.Google Scholar

Aydin, A., and Johnson, A. M. 1983. Analysis of faulting in porous sandstones. J. Struct. Geol. 5(1): 19–31 doi: 10.1016/0191–8141(83)90004–4.Google Scholar

Aydin, A., and Nur, A. 1982. Evolution of pull-apart basins and their scale independence. Tectonics 1: 91–105.Google Scholar

Bai, T. X., and Pollard, D. D. 2000a. Fracture spacing in layered rocks: A new explanation based on the stress transition. J. Struct. Geol. 22(1): 43–57, doi: 10.1016/s0191-8141(99)00137–6.Google Scholar

Bai, T. X., Pollard, D. D., and Gao, H. J. 2000b. Spacing of edge fractures in layered materials. Int. J. Fract. 103(4): 373–395, doi: 10.1023/a:1007659406011.Google Scholar

Baisch, S., Vörös, R., Rothert, E., Stang, H., Jung, R., and Schellschmidt, R. 2010. A numerical model for fluid injection induced seismicity at Soultz-sous-Forêts. Int. J. Rock Mech. Min. Sci. 47(3): 405–413.Google Scholar

Bak, J., Korstgard, J. and Sorensen, K. 1975. Major shear zone within Nagssugtoqidian of West Greenland. Tectonophysics 27(3): 191–209.Google Scholar

Bak, P., and Tang, C. 1989. Earthquakes as a self-organized critical phenomenon. J. Geophys. Res. 94: 15635–15637.Google Scholar

Bak, P., Tang, C., and Weisenfeld, K. 1987. Self-organized criticality: An explanation of l/f noise. Phys. Rev. Lett. 59: 381–384.Google Scholar

Bak, P., Tang, C., and Wiesenfeld, K. 1988. Self-organized criticality. Phys. Rev. A 38: 364–374.Google Scholar

Baker, B. H., and Wohlenberg, J. 1971. Structure and evolution of the Kenya rift valley. Nature 229: 538.Google Scholar

Bakun, W. H., and Lindh, A. 1985. The Parkfield, California, earthquake prediction experiment. Science 229: 619–624.Google Scholar

Bakun, W. H., and McEvilly, T. V. 1984. Recurrence models and Parkfield, California, earthquakes. J. Geophys. Res. 89: 3051–3058.Google Scholar

Bakun, W. H., King, G. C. P., and Cockerham, R. S. 1986. Seismic slip, aseismic slip, and the mechanics of repeating earthquakes on the Calaveras fault, California. In Earthquake Source Mechanics. Geophys, AGU. Mono. 37, eds. Das, S., Scholz, C., and Boatwright, J.. Washington, DC: American Geophysical Union, pp. 195–207.Google Scholar

Bakun, W. H., Stewart, R. M., Bufe, C. G., and Marks, S. M. 1980. Implication of seismicity for failure of a section of the San Andreas fault. Bull. Seismol. Soc. Amer. 70: 185–201.Google Scholar

Bakun, W., Aagaard, B., Dost, B., et al. 2005. Implications for prediction and hazard assessment from the 2004 Parkfield earthquake. Nature 437(7061): 969–974.Google Scholar

Baltay, A. S., Hanks, T. C., and Beroza, G. C. 2013. Stable Stress-Drop Measurements and their Variability: Implications for Ground-Motion Prediction. Bull. Seismol. Soc. Amer. 103: 211–222, doi: 10.1785/0120120161.Google Scholar

Banerjee, P., Pollitz, F. F., and Bürgmann, R. 2005. The size and duration of the Sumatra-Andaman earthquake from far-field static offsets. Science 308(5729): 1769–1772.Google Scholar

Barbot, S., Lapusta, N., and Avouac, J.-P. 2012. Under the hood of the earthquake machine: Toward predictive modeling of the seismic cycle. Science 336(6082): 707–710.CrossRefGoogle ScholarPubMed

Barenblatt, G. I. 1962. The mathematical theory of equilibrium cracks in brittle fracture. Adv. Appl. Mech. 7: 55–80.Google Scholar

Barka, A., and Kadinsky-Cade, K. 1988. Strike-slip fault geometry in Turkey and its influence on earthquake activity. Tectonics 7: 663–684.Google Scholar

Barnett, D. E., Bowman, J. R., Pavlis, T. L., Rubenstone, J. R., Snee, L. W., and Onstott, T. C. 1994. Metamorphism and near-trench plutonism during initial accretion of the cretaceous Alaskan fore-arc. J. Geophys. Res.-Solid Earth 99: 24007–24024.Google Scholar

Barnett, J. A., Mortimer, J., Rippon, J. H., Walsh, J. J., and Watterson, J. 1987. Displacement geometry in the volume containing a single normal fault. Am. Assoc. Pet. Geol. Bull. 71: 925–937.Google Scholar

Barnhart, W. D. 2017. Fault creep rates of the Chaman fault (Afghanistan and Pakistan) inferred from InSAR. J. Geophys. Res.-Solid Earth, 122: 372–386, doi: 10.1002/2016JB013656.Google Scholar

Barr, T. D., and Dahlen, F. A. 1989. Brittle frictional mountain building 2. Thermal structure and heat budget. J. Geophys. Res. 94: 3923–3947.Google Scholar

Barton, C. A., Zoback, M. D., and Moos, D. 1995. Fluid-flow along potentially active faults in crystalline rock. Geology 23: 683–686.Google Scholar

Bassett, D., Sutherland, R., and Henrys, S. 2014. Slow wavespeeds and fluid overpressure in a region of shallow geodetic locking and slow slip, Hikurangi subduction margin. Earth Planet. Sci. Lett. 389: 1–13.Google Scholar

Baud, P., and Meredith, P. G. 1997. Damage accumulation during triaxial creep of Darley Dale sandstone from pore volumometry and acoustic emission. Int. J. Rock Mech. Min. Sci. 34: 3–4.Google Scholar

Baumberger, T., and Caroli, C. 2006. Solid friction from stick-slip down to pinning and aging. Adv. Phys. 55(3–4): 279–348, doi: 10.1080/00018730600732186.Google Scholar

Baumberger, T., Berthoud, P., and Caroli, C. 1999. Physical analysis of the state- and rate-dependent friction law. II. Dynamic friction. Phys. Rev. B-Condens Matter 60(6): 3928–3939.Google Scholar

Beach, A., Welbon, A. I., Brockbank, P. J., and McCallum, J. E. 1999. Reservoir damage around faults: Outcrop examples from the Suez rift. Petrol. Geosci. 5(2): 109–116, doi: 10.1144/petgeo.5.2.109.Google Scholar

Beavan, J., Bilham, R., and Hurst, K. 1984. Coherent tilt signals observed in the Shumagin seismic gap: Detection of time-dependent subduction at depth? J. Geophys. Res. 89: 4478–4492.Google Scholar

Beavan, J., Wang, X., Holden, C., Wilson, K., Power, W., Prasetya, G., Bevis, M., and Kautoke, R. 2010. Near-simultaneous great earthquakes at Tongan megathrust and outer rise in September 2009. Nature 466(7309): 959–978, doi: 10.1038/nature09292.Google Scholar

Bécel, A., Delescluse, M., Nedimović,  M. R., et al. 2017. Tsunamigenic structures in a creeping section of the Alaska subduction zone. Nat. Geosci. 10: 609–613, doi: 10.1038/ngeo2990.Google Scholar

Beeler, N. M., and Lockner, D. A. 2003. Why earthquakes correlate weakly with the solid Earth tides: Effects of periodic stress on the rate and probability of earthquake occurrence. J. Geophys. Res.-Solid Earth 108(B8): doi: 10.1029/2001jb001518.Google Scholar

Beeler, N. M., Hickman, S. H., and Wong, T. F. 2001. Earthquake stress drop and laboratory-inferred interseismic strength recovery. J. Geophys. Res. 106: 30701–30713Google Scholar

Beeler, N. M., Hirth, G., Thomas, A., and Buergmann, R. 2016. Effective stress, friction, and deep crustal faulting. J. Geophys. Res.-Solid Earth 121(2): 1040–1059, doi: 10.1002/2015jb012115.Google Scholar

Beeler, N. M., Lockner, D. L., and Hickman, S. H. 2001. A simple stick-slip and creep-slip model for repeating earthquakes and its implication for microearthquakes at Parkfield. Bull. Seismol. Soc. Am. 91(6): 1797–1804, doi: 10.1785/0120000096.Google Scholar

Beeler, N. M., Tullis, T. E., and Goldsby, D. L. 2008. Constitutive relationships and physical basis of fault strength due to flash heating. J. Geophys. Res.-Solid Earth 113(B1): doi: 10.1029/2007jb004988.Google Scholar

Beeler, N. M., Tullis, T. E., and Weeks, J. D. 1994. The roles of time and displacement in the evolution effect in rock friction. Geophys. Res. Lett. 21: 1987–1990.Google Scholar

Behr, W. M., and Platt, J. P. 2011. A naturally constrained stress profile through the middle crust in an extensional terrane. Earth Planet. Sci. Lett. 303(3–4): 181–192, doi: 10.1016/j.epsl.2010.11.044.Google Scholar

Belardinelli, M. E., Bonafede, M., and Gudmundsson, A. 2000. Secondary earthquake fractures generated by a strike-slip fault in the South Iceland Seismic Zone. J. Geophys. Res. 105: 13613–13630.Google Scholar

Belardinelli, M. E., Cocco, M., Coutant, O., and Cotton, F. 1999. Redistribution of dynamic stress during coseismic ruptures: Evidence for fault interaction and earthquake triggering. J. Geophys. Res.-Solid Earth 104: 14925–14945.Google Scholar

Bell, J. W., Caskey, S. J., Ramelli, A. R., and Guerrieri, l. 2004. Pattern and rates of faulting in the central Nevada seismic belt, and paleoseismic evidence for prior beltlike behavior. Bull. Seismol. Soc. Amer. 94: 1229–1254.Google Scholar

Bell, M. L., and Nur, A. 1978. Strength changes due to reservoir induced pore pressure and stresses and application to Lake Oroville. J. Geophys. Res. 83: 4469–4483.Google Scholar

Bell, T. H., and Etheridge, M. A. 1973. Microstructures of mylonites and their descriptive terminology. Lithos 6: 337–348.Google Scholar

Ben-David, O., and Fineberg, J. 2011. Static friction coefficient is not a material constant. Phys. Rev. Lett. 106(25): doi: 10.1103/PhysRevLett.106.254301.Google Scholar

Ben-David, O., Cohen, G., and Fineberg, J. 2010a. The dynamics of the onset of frictional slip. Science 330(6001): 211–214, doi: 10.1126/science.1194777.Google Scholar

Ben-David, O., Rubinstein, S. M., and Fineberg, J. 2010b. Slip-stick and the evolution of frictional strength. Nature 463(7277): 76–79, doi: 10.1038/nature08676.Google Scholar

Bennett, M., Schatz, M. F., Rockwood, H., and Wiesenfeld, K. 2002. Huygens’s clocks. P. Roy. Soc. A-Math. Phy, 458(2019), 563–579, doi: 10.1098/rspa.2001.0888.Google Scholar

Bennett, R. A., Davis, J. L., and Wernicke, B. P. 1999. Present-day pattern of Cordilleran deformation in the western United States. Geology 27: 371–374.Google Scholar

Bennett, R. A., Rodi, W., and Reilinger, R. 1996. Global Positioning System constraints on fault slip rates in southern California and northern Baja, Mexico. J. Geophys. Res. 101: 21, 943–21, 960.Google Scholar

Ben-Zion, Y., and Rice, J. R. 1993. Earthquake failure sequences along a cellular fault zone in a 3-dimensional elastic solid containing asperity and non-asperity regions. J. Geophys. Res.-Solid Earth 98(B8): 14109–14131, doi: 10.1029/93jb01096.Google Scholar

Ben-Zion, Y., and Rice, J. R. 1995. Slip patterns and earthquake populations along different classes of faults in elastic solids. J. Geophys. Res.-Solid Earth 100: 12959–12983.Google Scholar

Ben-Zion, Y., and Shi, Z. Q. 2005. Dynamic rupture on a material interface with spontaneous generation of plastic strain in the bulk. Earth Planet. Sci. Lett. 236(1–2): 486–496, doi: 10.1016/j.epsl.2005.03.025.Google Scholar

Ben-Zion, Y., Rice, J. R., and Dmowska, R. 1993. Interaction of the San Andreas fault creeping segment with adjacent great rupture zones and earthquake recurrence at Parkfield. J. Geophys. Res. 98: 2134–2144.Google Scholar

Bergman, E. A. 1986. Intraplate earthquakes and the state of stress in oceanic lithosphere. Tectonophysics 132: 1–35.Google Scholar

Bergman, E. A., and Solomon, S. 1988. Transform fault earthquakes in the North Atlantic: Source mechanism and depth of faulting. J. Geophys. Res. 93: 9027–9057.Google Scholar

Bergman, E. A., and Solomon, S. C. 1980. Oceanic intraplate earthquakes – Implications for local and regional intraplate stress. J. Geophys. Res. 85(NB10): 5389–5410, doi: 10.1029/JB085iB10p05389.Google Scholar

Berkhemer, H., Zschau, J., and Ergunay, O. 1988. The German-Turkish project on earthquake prediction research, concept and first results. Paper presented at Proceedings of the ECE/UN Seminar on Prediction of Earthquakes, Lisbon.Google Scholar

Beroza, G. C. 1991. Near-source modeling of the Loma-Prieta earthquake – Evidence for heterogeneous slip and implications for earthquake hazard. Bull. Seismol. Soc. Amer. 81: 1603–1621.Google Scholar

Beroza, G. C., and Ide, S. 2011. Slow Earthquakes and Nonvolcanic Tremor. In Ann. Rev. Earth Planet. Sci, Vol 39, eds. R. Jeanloz and K. H. Freeman, pp. 271–296, doi: 10.1146/annurev-earth-040809–152531.Google Scholar

Beroza, G. C., and Mikumo, T. 1996. Short slip duration in dynamic rupture in the presence of heterogeneous fault properties. J. Geophys. Res.-Solid Earth 101(B10): 22449–22460, doi: 10.1029/96jb02291.Google Scholar

Berthaud, P., Baumberger, T., G’sell, C., and Hiver, J. M. 1999. Physical analysis of the state and rate-dependent friction law: Static friction. Phys. Rev. B. 59: 14313.Google Scholar

Berthe, D., Choukroune, P., and Jegouzo, P. 1979. Orthogneiss, mylonite and non-coaxial deformation of granites: The example of the South Armorican shear zone. J. Struct. Geol. 1: 31–42.Google Scholar

Bhat, H. S., Dmowska, R., Rice, J. R., and Kame, N. 2004. Dynamic slip transfer from the Denali to Totschunda faults, Alaska: Testing theory for fault branching. Bull. Seismol. Soc. Am. 94(6): S202–S213, doi: 10.1785/0120040601.Google Scholar

Bhattacharya, P., Rubin, A. M., Bayart, E., Savage, H. M., and Marone, C. 2015. Critical evaluation of state evolution laws in rate and state friction: Fitting large velocity steps in simulated fault gouge with time-, slip-, and stress-dependent constitutive laws. J. Geophys. Res.-Solid Earth 120(9): 6365–6385, doi: 10.1002/2015jb012437.Google Scholar

Biasi, G. P., and Wesnousky, S. 2017. Bends and ends of surface ruptures. Bull. Seismol. Soc. Amer. 107: 2543–2560, doi: 10.1785/0120160292.Google Scholar

Biasi, G. P., and Wesnousky, S. G. 2016. Steps and gaps in ground ruptures: Empirical bounds on rupture propagation. Bull. Seismol. Soc. Am. 106(3): 1110–1124, doi: 10.1785/0120150175.Google Scholar

Biegel, R. L., Wang, W., Scholz, C. H., Boitnott, G. N., and Yoshioka, N. 1992. Micromechanics of rock friction. 1. Effects of surface-roughness on initial friction and slip hardening in westerly granite. J. Geophys. Res.-Solid Earth 97: 8951–8964.Google Scholar

Bilek, S. L. 2010. The role of subduction erosion on seismicity. Geology 38(5): 479–480, doi: 10.1130/focus052010.1.Google Scholar

Bilek, S. L., and Engdahl, E. R. 2007. Rupture characterization and aftershock relocations for the 1994 and 2006 tsunami earthquakes in the Java subduction zone. Geophys. Res. Lett. 34(20): doi: 10.1029/2007gl031357.Google Scholar

Bilek, S. L., and Lay, T. 2002. Tsunami earthquakes possibly widespread manifestations of frictional conditional stability. Geophys. Res. Lett. 29(14): doi: 10.1029/2002gl015215.Google Scholar

Bilek, S. L., Engdahl, E. R., DeShon, H. R., and El Hariri, M. 2011. The 25 October 2010 Sumatra tsunami earthquake: Slip in a slow patch. Geophys. Res. Lett. 38, doi: 10.1029/2011gl047864.Google Scholar

Bilham, R. G., and Beavan, J. 1978. Tilts and strains on crustal blocks. Tectonophysics 52: 121–138.Google Scholar

Bilham, R. G., and Williams, P. 1985. Sawtooth segmentation and deformation processes on the southern San Andreas fault, California. Geophys. Res. Lett. 12: 557–560.Google Scholar

Bilham, R., and Yu, T. T. 2000. The morphology of thrust faulting in the 21 September 1999, Chichi, Taiwan earthquake. J. Asian Earth Sci. 18(3): 351–367, doi: 10.1016/s1367-9120(99)00071–1.Google Scholar

Bilham, R., Engdahl, R., Feldl, N., and Satyabala, S. P. 2005. Partial and complete rupture of the Indo-Andaman plate boundary 1847–2004. Seismol. Res. Lett. 76(3): 299–311.Google Scholar

Bilham, R., Ozener, H., Mencin, D., et al. 2016. Surface creep on the North Anatolian Fault at Ismetpasa, Turkey, 1944–2016, J. Geophys. Res., 121, doi: 10.1002/2016JB013394.Google Scholar

Bird, P., Kagan, Y. Y., and Jackson, D. D. 2002. Plate tectonics and earthquake potential of spreading ridges and oceanic transform faults, Wiley Online Library: https://doi.org/10.1029/GD030p0203.Google Scholar

Bizzarri, A. 2010. Pulse-like dynamic earthquake rupture propagation under rate-, state- and temperature-dependent friction. Geophys. Res. Lett. 37, doi: 10.1029/2010gl044541.Google Scholar

Bjarnason, I. T., Cowie, P., Anders, M. H., Seeber, L., and Scholz, C. H. 1993. The 1912 Iceland earthquake rupture – Growth and development of a nascent transform system. Bull. Seismol. Soc. Amer. 83: 416–435.Google Scholar

Blanpied, M. L., Lockner, D. A., and Byerlee, J. D. 1992. An earthquake mechanism based on rapid sealing of faults. Nature 358: 574–6.Google Scholar

Blanpied, M. L., Lockner, D. A., and Byerlee, J. D. 1995. Frictional slip of granite at hydrothermal conditions. J. Geophys. Res.-Solid Earth 100: 13045–13064.Google Scholar

Blanpied, M. L., Marone, C. J., Lockner, D. A., Byerlee, J. D., and King, D. P. 1998. Quantitative measure of the variation in fault rheology due to fluid-rock interactions. J. Geophys. Res. 103: 9691–9712.Google Scholar

Blenkinsop, T. G. 1989. Thickness – Displacement relationships for deformation zones: Discussion, J. Struct. Geol., 8: 1051–1054.Google Scholar

Boatwright, J. 1980. A spectral theory for circular seismic sources: Simple estimates of source dimension, dynamic stress-drop and radiated seismic energy. Bull Seismol. Soc. Am. 70: 1–27.Google Scholar

Boatwright, J. 1985. Characteristics of the aftershock sequence of the Borah Peak, Idaho, earthquake determined from digital recordings of the events. Bull. Seismol. Soc. Am. 75: 1265–1284.Google Scholar

Boatwright, J., and Choy, G. L. 1986. Teleseismic estimates of the energy radiated by shallow earthquakes. J. Geophys. Res.-Solid Earth and Planets 91(B2): 2095–2112, doi: 10.1029/JB091iB02p02095.Google Scholar

Bodin, P., and Brune, J. N. 1996. On the scaling of slip with rupture length for shallow strike-slip earthquakes: Quasi-static models and dynamic rupture propagation. Bull. Seismol. Soc. Amer. 86: 1292–1299.Google Scholar

Bodin, P., Bilham, R., Behr, J., Gomberg, J., and Hudnut, K. W. 1994. Slip triggered on southern California faults by the 1992 Joshua-Tree, Landers, and Big-Bear earthquakes. Bull. Seismol. Soc. Amer. 84: 806–816.Google Scholar

Boettcher, M. S., and Jordan, T. H. 2004. Earthquake scaling relations for mid-ocean ridge transform faults. J. Geophys. Res.-Solid Earth 109(B12), doi: 10.1029/2004jb003110.Google Scholar

Boettcher, M. S., and McGuire, J. J. 2009. Scaling relations for seismic cycles on mid-ocean ridge transform faults. Geophys. Res. Lett. 36, doi: 10.1029/2009gl040115.Google Scholar

Boettcher, M. S., Hirth, G., and Evans, B. 2007. Olivine friction at the base of oceanic seismogenic zones. J. Geophys. Res.-Solid Earth 112(B1): doi: 10.1029/2006jb004301.Google Scholar

Bohnenstiehl, D. R., Tolstoy, M., and Chapp, E. 2004. Breaking into the plate: A 7.6 Mw fracture-zone earthquake adjacent to the Central Indian Ridge. Geophys. Res. Lett. 31(2): doi: 10.1029/2003gl018981.Google Scholar

Boitnott, G. N., Biegel, R. L., Scholz, C. H., Yoshioka, N., and Wang, W. 1992. Micromechanics of rock friction 2. Quantitative modeling of initial friction with contact theory. J. Geophys. Res.-Solid Earth 97: 8965–8978.Google Scholar

Boland, J. N., and Tullis, T. E. 1986. Deformation behavior of wet and dry clinopyroxenite in the brittle to ductile transition region. In Mineral and Rock Deformation: Laboratory Studies AGU Geophys. Mono, eds. Hobbs, B. E. and Heard, H. C.. Washington, DC: American Geophysical Union, pp. 35–50.Google Scholar

Bolt, B. A. 1978. Earthquakes: A Primer. San Francisco: Freeman.Google Scholar

Boncio, P., Pizzi, A., Brozzetti, F., Pomposo, G., Lavecchia, G., Di Naccio, D., and Ferrarini, F. 2010. Coseismic ground deformation of the 6 April 2009 L’Aquila earthquake. central Italy, M(w)6.3, Geophys. Res. Lett., 37, doi: 10.1029/2010gl042807.Google Scholar

Boneh, Y, and Reches, Z. 2017. Geotribology – Friction, wear, and lubrication of faults. Tectonophysics 733: 171–181: doi: 10.1016/jtecto.2017.11.022.Google Scholar

Boneh, Y., Chang, J. C., Lockner, D. A., and Reches, Z. 2014. Evolution of wear and friction along experimental faults. Pure Appl. Geophys, 171(11): 3125–3141, doi: 10.1007/s00024-014–0801-3.Google Scholar

Boneh, Y., Sagy, A., and Reches, Z. 2013. Frictional strength and wear-rate of carbonate faults during high-velocity, steady-state sliding, Earth Planet. Sci. Lett. 381: 127–137, doi: 10.1016/j.epsl.2013.08.050.Google Scholar

Borghi, A., Aoudia, A., Javed, F., and Barzaghi, R. 2016. Precursory slow-slip loaded the 2009 L’Aquila earthquake sequence, Geophys. J. Int., 205(2): 776–784, doi: 10.1093/gji/ggw046.Google Scholar

Bos, B., and Spiers, C. J. 2000. Effect of phyllosilicates on fluid-assisted healing of gouge-bearing faults. Earth Planet. Sci. Lett. 184(1): 199–210, doi: 10.1016/s0012-821x(00)00304–6.Google Scholar

Bos, B., and Spiers, C. J. 2002. Frictional-viscous flow of phyllosilicate-bearing fault rock: Microphysical model and implications for crustal strength profiles. J. Geophys. Res.-Solid Earth 107(B2): 2028, doi: 10.1029/2001jb000301.Google Scholar

Bose, M., Allen, R., Brown, H., et al. 2014. CISN ShakeAlert: An Earthquake Early Warning demonstration systme for California. In Early Warnings for Geological Disasters – Scientific methods and Current Practice, ed. Zschau, E. W. A. J., Springer, Berlin, Germany.Google Scholar

Böse, M., Felizardo, C., and Heaton, T. H. 2015. Finite-fault rupture detector (FinDer): Going real-time in Californian ShakeAlert warning system. Seismol. Res. Lett. 86(6): 1692–1704.Google Scholar

Bouchon, M. 1982. The rupture mechanism of the Coyote Lake earthquake of 6 Aug. 1979 inferred from near field data. Bull. Seismol. Soc. Amer. 72: 745–757.Google Scholar

Bouchon, M. 1997. The state of stress on some faults of the San Andreas system as inferred from near-field strong motion data. J. Geophys. Res. 102: 11731–11744.Google Scholar

Bouchon, M., Bouin, M. P., Karabulut, H., Toksoz, M. N., Dietrich, M., and Rosakis, A. J. 2001. How fast is rupture during an earthquake? New insights from the 1999 Turkey earthquakes. Geophys. Res. Lett. 28(14): 2723–2726, doi: 10.1029/2001gl013112.Google Scholar

Bouchon, M., Campillo, M., and Cotton, F. 1998. Stress field associated with the rupture of the 1992 Landers, California, earthquake and its implications concerning the fault strength at the onset of the earthquake. J. Geophys. Res. 103: 21091–21097.Google Scholar

Bouchon, M., Durand, V., Marsan, D., Karabulut, H., and Schmittbuhl, J. 2013. The long precursory phase of most large interplate earthquakes. Nat Geosci. 6(4): 299–302, doi: 10.1038/ngeo1770.Google Scholar

Bouchon, M., Karabulut, H., Aktar, M., Ozalaybey, S., Schmittbuhl, J., and Bouin, M. P. 2011. Extended Nucleation of the 1999 Mw Izmit Earthquake. Science 331: 878–882.Google Scholar

Bouchon, M., Karabulut, H., Bouin, M. P et al. 2010. Faulting characteristics of supershear earthquakes. Tectonophysics 493(3–4): 244–253, doi: 10.1016/j.tecto.2010.06.011.Google Scholar

Bouchon, M., Marsan, D., Durand, V., et al. 2016. Potential slab deformation and plunge prior to the Tohoku, Iquique and Maule earthquakes. Nat. Geosci. 9(5): 380+, doi: 10.1038/ngeo2701.Google Scholar

Bourne, S. J., Arnadottir, T., Beavan, J., et al. 1998. Crustal deformation of the Marlborough fault zone in the South Island of New Zealand: Geodetic constraints over the interval 1982–1994. J. Geophys. Res.-Solid Earth 103: 30147–30165.Google Scholar

Bourne, S. J., England, P. C., and Parsons, B. 1998. The motion of crustal blocks driven by flow of the lower lithosphere and implications for slip rates of continental strike-slip faults. Nature 391: 655–659.Google Scholar

Bowden, F. P., and Tabor, D. 1950. The Friction and Lubrication of Solids: Part 1. Oxford: Clarendon Press.Google Scholar

Bowden, F. P., and Tabor, D. 1964. The Friction and Lubrication of Solids. Part II. Oxford: Clarendon Press.Google Scholar

Bowman, D. D., Ouillon, G., Sammis, C. G., Sornette, A., and Sornette, D. 1998. An observational test of the critical earthquake concept. J. Geophys. Res.-Solid Earth 103: 24359–24372.Google Scholar

Bowman, J., Jones, T., Gibson, G., Corke, A., Thompson, R., and Comacho, A. 1988. Tennant Creek earthquakes of 22 January 1988: Reactivation of a fault zone in the Proterozoic Australian shield. Eos 69: 400.Google Scholar

Brace, W. F. 1960. An extension of the Griffith theory of fracture to rocks. J. Geophys. Res. 65: 3477–3480.CrossRefGoogle Scholar

Brace, W. F. 1961. Dependence of the fracture strength of rocks on grain size. Penn. State Univ. Min. Ind. Bull. 76: 99–103.Google Scholar

Brace, W. F. 1963. Behavior of quartz during indentation. J. Geol. 71(5): 581–595.Google Scholar

Brace, W. F. 1972. Laboratory studies of stick-slip and their application to earthquakes. Tectonophysics 14: 189–200.Google Scholar

Brace, W. F. 1980. Permeability of crystalline and argillaceous rocks. Int. J. Rock Mech. Min. Sci. 17: 241–251.Google Scholar

Brace, W. F. 1984. Permeability of crystalline rocks – New in situ measurements. J. Geophys. Res. 89 (NB6): 4327–4330.Google Scholar

Brace, W. F., and Bombalakis, E. G. 1963. A note on brittle crack growth in compression. J. Geophys. Res. 68: 3709–3713.Google Scholar

Brace, W. F., and Byerlee, J. D. 1966. Stick slip as a mechanism for earthquakes. Science 153: 990–992.Google Scholar

Brace, W. F., and Byerlee, J. D. 1970. California earthquakes – Why only shallow focus? Science 168: 1573–1575.Google Scholar

Brace, W. F., and Kohlstedt, D. 1980. Limits on lithospheric stress imposed by laboratory experiments. J. Geophys. Res. 85: 6248–6252.Google Scholar

Brace, W. F., and Martin, R. J. 1968. A test of the law of effective stress for crystalline rocks of low porosity. Int. J. Rock Mech. Min. Sci. 5: 415–426.Google Scholar

Brace, W. F., and Walsh, J. B. 1962. Some direct measurements of the surface energy of quartz and orthoclase. Am. Mineral 47: 1111–1122.Google Scholar

Brace, W. F., Paulding, B. W., and Scholz, C. H. 1966. Dilatancy in the fracture of crystalline rocks. J. Geophys. Res. 71: 3939–3953.Google Scholar

Brady, B. T. 1969. A statistical theory of brittle fracture of rock materials. Int. J. Rock Mech. Min. Sci. I. 6: 21–42.Google Scholar

Brantut, N., Heap, M. J., Baud, P., and Meredith, P. G. 2014. Rate- and strain-dependent brittle deformation of rocks. J. Geophys. Res.-Solid Earth 119(3): 1818–1836, doi: 10.1002/2013jb010448.Google Scholar

Brantut, N., Heap, M. J., Meredith, P. G., and Baud, P. 2013. Time-dependent cracking and brittle creep in crustal rocks: A review. J. Struct. Geol. 52: 17–43, doi: 10.1016/j.jsg.2013.03.007.Google Scholar

Brantut, N., Schubnel, A., Corvisier, J., and Sarout, J. 2010. Thermochemical pressurization of faults during coseismic slip. J. Geophys. Res.-Solid Earth 115, doi: 10.1029/2009jb006533.Google Scholar

Brantut, N., Stefanou, I., and Sulem, J. 2017. Dehydration-induced instabilities at intermediate depths in subduction zones. J. Geophys. Res.-Solid Earth 122(8): 6087–6107, doi: 10.1002/2017jb014357.Google Scholar

Braunmiller, J., and Nabelek, J. 1996. Geometry of continental normal faults: Seismological constraints. J. Geophys. Res.-Solid Earth 101: 3045–3052.Google Scholar

Braunmiller, J., and Nabelek, J. 2008. Segmentation of the Blanco Transform Fault Zone from earthquake analysis: Complex tectonics of an oceanic transform fault. J. Geophys. Res.-Solid Earth 113(B7): doi: 10.1029/2007jb005213.Google Scholar

Brechet, Y., and Estrin, Y. 1994. The effect of strain rate sensitivity on dynamic friction of metals, Scripta Met. Mater. 30: 1449–1454.Google Scholar

Bridgman, P. W. 1945. Polymorphic transitions and geological phenomena. Am. J. Sci. 243A: 90–97.Google Scholar

Briggs, R. W., Sieh, K., Meltzner, A. J., et al. Deformation and slip along the Sunda megathrust in the great 2005 Nias-Simeulue earthquake. Science 311(5769): 1897–1901.Google Scholar

Brock, N. G. and Engelder, T. 1977. Deformation associated with movement of Muddy Mountain overthrust in Buffington Window, Southeastern Nevada. Geol. Soc. Am. Bull. 88 (11): 1667–1677.Google Scholar

Brodsky, E. E. 2006. Long-range triggered earthquakes that continue after the wave train passes. Geophys. Res. Lett. 33(15): L15313, doi: 10.1029/2006gl026605.Google Scholar

Brodsky, E. E., and Kanamori, H. 2001. Elastohydrodynamic lubrication of faults. J. Geophys. Res.-Solid Earth 106(B8): 16357–16374, doi: 10.1029/2001jb000430.Google Scholar

Brodsky, E. E., and Mori, J. 2007. Creep events slip less than ordinary earthquakes. Geophys. Res. Lett. 34: L16309, doi: 16310.11029/12007GL030917.Google Scholar

Brodsky, E. E., and van der Elst, N. J. 2014. The Uses of Dynamic Earthquake Triggering. In Ann. Rev. Earth Planet. Sci. Vol 42, ed. R. Jeanloz, pp. 317–339, doi: 10.1146/annurev-earth-060313–054648.Google Scholar

Brodsky, E. E., Gilchrist, J. J., Sagy, A., and Collettini, C. 2011. Faults smooth gradually as function of slip. Earth Planet. Sci. Lett. 302(1–2): 185–193, doi: 10.1016/j.epsl.2010.12.010.Google Scholar

Brodsky, E. E., Kirkpatrick, J. D., and Candela, T. 2016. Constraints from fault roughness on the scale-dependent strength of rocks. Geology 44(1): 19–22.Google Scholar

Brown, K. M., and Fialko, Y. 2012. “Melt welt” mechanism of extreme weakening of gabbro at seismic slip rates. Nature 488: 638–641, doi: 10.1038/nature11370.Google Scholar

Brown, S. R., and Scholz, C. H. 1985a. Closure of random elastic surfaces in contact. J. Geophys. Res. 90: 5531–5545.Google Scholar

Brown, S. R., and Scholz, C. H. 1985b. Broad bandwidth study of the topography of natural rock surfaces. J. Geophys. Res. 90: 12575–12582.Google Scholar

Brown, S. R., and Scholz, C. H. 1986. Closure of rock joints. J. Geophys. Res. 91: 4939–4948.Google Scholar

Brown, S. R., Scholz, C. H., and Rundle, J. B. 1991. A simplified spring-block model of earthquakes. Geophys. Res. Lett. 18, 215–18,218:Google Scholar

Brudy, M., Zoback, M. D., Fuchs, K., Rummel, F., and Baumgartner, J. 1997. Estimation of the complete stress tensor to 8 km depth in the KTB scientific drill holes: Implications for crustal strength. J. Geophys. Res.-Solid Earth 102: 18453–18475.Google Scholar

Brudzinski, M. R., Thurber, C. H., Hacker, B. R., and Engdahl, E. R. 2007. Global prevalence of double Benioff zones. Science 316(5830): 1472–1474, doi: 10.1126/science.1139204.Google Scholar

Bruhat, L., Barbot, S., and Avouac, J.-P. 2011. Evidence for postseismic deformation of the lower crust following the 2004 Mw6.0 Parkfield earthquake. J. Geophys. Res.-Solid Earth 116, doi: 10.1029/2010jb008073.Google Scholar

Brun, J. P., and Cobbold, P. R. 1980. Strain heating and thermal softening in continental shear zones: A review. J. Struct. Geol. 2: 149–158.Google Scholar

Brune, J. 1968. Seismic moment, seismicity, and rate of slip along major fault zones. J. Geophys. Res. 73: 777–784.Google Scholar

Brune, J. 1970. Tectonic stress and the spectra of seismic shear waves from earthquakes. J. Geophys. Res. 75: 4997–5009.Google Scholar

Brune, J. N. 1996. Particle motions in a physical model of shallow angle thrust faulting. P. Indian As-Math. Sci. -- Earth and Planetary Sciences 105(2): L197–L206.Google Scholar

Brune, J. N. 2001. Fault normal dynamic loading and unloading: An explanation for “non-gouge” rock powder and lack of fault-parallel shear bands along the San Andreas Fault; EOS Transactions, American Geophysical Union. AGU Fall Meeting Abstracts. 8. 0655.Google Scholar

Brune, J. N., Brown, S., and Johnson, P. A. 1993. Rupture mechanism and interface separation in foam rubber models of earthquakes – A possible solution to the heat flow paradox and the paradox of large overthrusts. Tectonophysics 218(1–3): 59–67, doi: 10.1016/0040–1951(93)90259-m.Google Scholar

Brune, J., Henyey, T., and Roy, R. 1969. Heat flow, stress, and rate of slip along the San Andreas fault, California. J. Geophys. Res. 74: 3821–3827.Google Scholar

Bucholc, M., and Steacy, S. 2016. Tidal stress triggering of earthquakes in Southern California, Geophys. J. Int. 205(2) 681–693, doi: 10.1093/gji/ggw045.Google Scholar

Buck, W. R. 1988. Flexural rotation of normal faults. Tectonics 7: 959–973.Google Scholar

Buck, W. R., Lavier, L. L., and Poliakov, A. N. B. 2005. Modes of faulting at mid-ocean ridges, Nature, 434(7034): 719–723, doi: 10.1038/nature03358.Google Scholar

Bufe, C. G., and Varnes, D. J. 1993. Predictive modeling of the seismic cycle of the greater San Francisco Bay region. J. Geophys. Res.-Solid Earth 98: 9871–9883.Google Scholar

Burford, R. 1972. Continued slip on the Coyote Creek fault after the Borrego Mountain earthquake. In The Borrego Mountain Earthquake of April 9, 1968, ed. US Geol. Surv. Prof. Paper, pp. 105–111.Google Scholar

Burford, R. 1988. Retardations in fault creep rates before local moderate earthquakes along the San Andreas fault system, central California. Pageoph 126: 499–529.Google Scholar

Burford, R., and Harsh, P. W. 1980. Slip on the San Andreas fault in central California from alinement array surveys. Bull. Seismol. Soc. Am. 70: 1233–1261.Google Scholar

Burgmann, R., and Dresen, G. 2008. Rheology of the lower crust and upper mantle: Evidence from rock mechanics, geodesy, and field observations. Ann. Rev. Earth Planet. Sci. 38: 531–567, doi: 10.1146/annurev.earth.36.031207.124326.Google Scholar

Bürgmann, R., Pollard, D. D., and Martel, S. J. 1994. Slip distributions on faults – Effects of stress gradients, inelastic deformation, heterogeneous host-rock stiffness, and fault interaction. J. Struct. Geol. 16: 1675–1690.Google Scholar

Bürgmann, R., Rosen, P. A., and Fielding, E. J. 2000. Synthetic aperture radar interferometry to measure Earth’s surface topography and its deformation. Ann. Rev. Earth Planet. Sci. 28: 169–209, doi: 10.1146/annurev.earth.28.1.169.Google Scholar

Bürgmann, R., Schmidt, D., Nadeau, R. M., et al. 2000. Earthquake potential along the northern Hayward fault, California. Science 289: 1178–1182.Google Scholar

Burnley, P. C., Green, H. W., and Prior, D. J. 1991. Faulting associated with the olivine to spinel transformation in Mg2GeO4 and its implications for deep‐focus earthquakes. J. Geophys. Res.-Solid Earth 96(B1): 425–443.Google Scholar

Burr, N., and Solomon, S. 1978. The relationship of source parameters of oceanic transform earthquakes to plate velocity and transform length. J. Geophys. Res. 83: 1193–1205.Google Scholar

Burridge, R. 1973. Admissible speeds for plane strain self-similar shear cracks with friction but lacking cohesion. Geophys. J. R.A.S. 35: 439–455.Google Scholar

Burridge, R., and Knopoff, L. 1967. Model and theoretical seismicity. Bull. Seism. Soc. Amer. 57: 341–362.Google Scholar

Burroughs, S. M., and Tebbens, S. F. 2001. Upper-truncated power laws in natural systems. Pure Appl. Geophys. 158(4): 741–757.Google Scholar

Byerlee, J. D. 1967a. Frictional characteristics of granite under high confining pressure. J. Geophys. Res. 72: 3639–3648.Google Scholar

Byerlee, J. D. 1967b. Theory of friction based on brittle fracture. J. Appl. Phys. 38: 2928–2934.Google Scholar

Byerlee, J. D. 1970. The mechanics of stick-slip. Tectonophysics 9: 475–486.Google Scholar

Byerlee, J. D. 1978. Friction of rocks. Pure Appl. Geophys. 116: 615–626.Google Scholar

Byerlee, J. D. 1990. Friction, overpressure, and fault normal compression. Geophys. Res. Lett. 17: 2109–12.Google Scholar

Byerlee, J. D., and Brace, W. F. 1968. Stick-slip, stable sliding, and earthquakes-effect of rock type, pressure, strain rate, and stiffness. J. Geophys. Res. 73: 6031–6037.Google Scholar

Byerlee, J. D., and Savage, J. C. 1992. Coulomb plasticity within the fault zone. Geophys. Res. Lett. 19: 2341–2344.Google Scholar

Bykov, V. G. 2014. Sine-Gordon equation and its application to tectonic stress transfer. J. Seismol. 18(3): 497–510, doi: 10.1007/s10950-014–9422-7.Google Scholar

Byrne, D. E., Davis, D. M., and Sykes, L. R. 1988. Loci and maximum size of thrust earthquakes and the mechanics of the shallow region of subduction zones. Tectonics 7: 833–857.Google Scholar

Cailleux, A. 1958. Etude quantitative de failles. Revue de Geomorphologie Dynamique IX(9–10): 129–145.Google Scholar

Caine, J. S., Evans, J. P., and Forster, C. B. 1996. Fault zone architecture and permeability structure. Geology 24: 1025–1028.Google Scholar

Camacho, A., Vernon, R. H., and Fitz Gerald, J. D. 1995. Large volumes of anhydrous pseudotachylyte in the Woodroffe Thrust, Eastern Musgrave Ranges, Australia, J. Struct. Geol., 17(3): 371–383.Google Scholar

Campos, J., Madariaga, R., and Scholz, C. H. 1996. Faulting process of the August 8, 1993 Guam earthquake: A thrust event in an otherwise weakly coupled subduction zone. J. Geophys. Res. 101: 17,581–17,596.Google Scholar

Campus, P., and Das, S. 2000. Comparison of the rupture and radiation characteristics of intermediate and deep earthquakes. J. Geophys. Res.-Solid Earth 105: 6177–6189.Google Scholar

Candela, T., and Brodsky, E. E. 2016. The minimum scale of grooving on faults. Geology 44(8): 603–606, doi: 10.1130/g37934.1.Google Scholar

Candela, T., Renard, F., Bouchon, M., Schmittbuhl, J., and Bodsky, E. E. 2011a. Stress Drop during Earthquakes: Effect of Fault Roughness Scaling. Bull. Seismol. Soc. Amer. 101: 2369–2387, doi: 10.1785/0120100298.Google Scholar

Candela, T., Renard, F., Klinger, Y., Mair, K., Schmittbuhl, J., and Brodsky, E. E. 2012. Roughness of fault surfaces over nine decades of length scales. J. Geophys. Res.-Solid Earth 117, doi: 10.1029/2011jb009041.Google Scholar

Candela, T., Renard, F., Schmittbuhl, J., Bouchon, M., and Brodsky, E. E. 2011b. Fault slip distribution and fault roughness. Geophys. J. Int. 187: 959–968, doi: 10.1111/j.1365-246X.2011.05189.x.Google Scholar

Cao, T., and Aki, K. 1985. Seismicity simulation with a mass-spring model and a displacement hardening-softening friction law. Pageoph 122: 10–23.Google Scholar

Cao, T., and Aki, K. 1986. Effect of slip rate on stress drop. Pageoph 124: 515–530.Google Scholar

Carder, D. S. 1945. Seismic investigations in the Boulder Dam area, 1940–1945, and the influence of reservoir loading on earthquake activity. Bull. Seismol. Soc. Am. 35: 175–192.Google Scholar

Cardwell, R. K., Chinn, D. S., Moore, G. F., and Turcotte, D. L. 1978. Frictional heating on a fault zone with finite thickness. Geophys. J. Roy. Astron. Soc. 52: 525–530.Google Scholar

Carlson, J. M., and Langer, J. S. 1989a. Properties of earthquakes generated by fault dynamics. Phys. Rev. Lett. 62: 2632–2635.Google Scholar

Carlson, J. M., and Langer, J. S. 1989b. Mechanical model of an earthquake fault. Phys. Rev. A 40: 6470–6484.Google Scholar

Carlson, R. L., Hilde, T. W. C., and Uyeda, S. 1983. The driving mechanism of plate tectonics – relation to age of the lithosphere at trenches. Geophys. Res. Lett. 10: 297–300.Google Scholar

Carpenter, B. M., Collettini, C., Viti, C., and Cavallo, A. 2016. The influence of normal stress and sliding velocity on the frictional behaviour of calcite at room temperature: Insights from laboratory experiments and microstructural observations. Geophys. J. Int. 205(1): 548–561, doi: 10.1093/gji/ggw038.Google Scholar

Carpenter, B. M., Saffer, D. M., and Marone, C.. 2015. Frictional properties of the active San Andreas Fault at SAFOD: Implications for fault strength and slip behavior. J. Geophys. Res.-Solid Earth 120(7): 5273–5289, doi: 10.1002/2015jb011963.Google Scholar

Carter, N. L., and Kirby, S. 1978. Transient creep and semi-brittle behavior of crystalline rocks. Pure Appl. Geophys. 116: 807–839.Google Scholar

Cartwright, J. A., Trudgill, B. D., and Mansfield, C. S. 1995. Fault growth by segment linkage – An explanation for scatter in maximum displacement and tracelength data from the Canyonlands graben of SE Utah. J. Struct. Geol. 17(9): 1319–1326, doi: 10.1016/0191–8141(95)00033-a.Google Scholar

Caskey, S. J., and Wesnousky, S. G. 1997. Static stress changes and earthquake triggering during the 1954 Fairview peak and Dixie valley earthquakes, central Nevada. Bull. Seismol. Soc. Amer. 87: 521–527.Google Scholar

Castillo, D., and Hickman, S. H. 2000. Systematic near-field stress rotations adjacent to the Carrizo Plain segment of the San Andreas fault, paper presented at Proceedings of the 3rd conference on tectonic problems of the San Andreas fault system, School of Earth Sciences, Stanford University.Google Scholar

Castle, R., Elliot, M., Church, J., and Wood, S. 1984. The Evolution of the Southern California Uplift, 1955 through 1976. In US Geol. Surv. Prof. Paper 1342.Google Scholar

Causse, M., Cotton, F., and Mai, P. M. 2010. Constraining the roughness degree of slip heterogeneity. J. Geophys. Res. 115, doi: 10.1029/2009JB006747.Google Scholar

Cembrano, J., Jensen, E., Griffith, W. A., Stanton-Yonge, A., Mitchell, T., and Anzaldo, Y. 2018. Self-similar displacement-lenth scaling of strike-slip faults in crystalline rocks: Mechanical implications. J. Struct. Geol. In print.Google Scholar

Cessaro, R. K., and Hussong, D. M. 1986. Transform seismicity at the intersection of the oceanographer fracture zone and the Mid-Atlantic ridge. J. Geophys. Res. 91: 4839–4853.Google Scholar

Cetin, E., Cakir, Z., Meghraoul, M., Ergintav, S., and Akoglu, A. M. 2014. Extent and distribution of aseismic slip on the Ismetpasa segment of the North Anatolian fault. turkey) from persistent scatterer in In SAR. Geochem. Geophys. Geosyst 15: 2883–2894 doi: 2810.1002/2014GC005307.Google Scholar

Challen, J. M., and Oxley, P. L. B. 1979. An explanation of the different regimes of friction and wear using asperity deformation models. Wear 53: 229–243.Google Scholar

Chaussard, E., Burgmann, R., Fattahi, H., Johnson, C. W., Nadeau, R., Taira, T., and Johanson, I. 2015. Interseismic coupling and refined earthquake potential on the Hayward-Calaveras fault zone. J. Geophys. Res.-Solid Earth 120(12): 8570–8590, doi: 10.1002/2015jb012230.Google Scholar

Cheloni, D., D’Agostino, N., D’Anastasio, E., et al. 2010. Coseismic and initial post-seismic slip of the 2009 M-w 6.3 L’Aquila earthquake, Italy, from GPS measurements. Geophys. J. Int. 181(3): 1539–1546, doi: 10.1111/j.1365-246X.2010.04584.x.Google Scholar

Chen, A., Frohlich, C., and Latham, G. 1982. Seismicity of the forearc marginal wedge (accretionary prism). J. Geophys. Res. 87: 3679–3690.Google Scholar

Chen, C. H., Tang, C.-C., Cheng, K.-C., et al. 2015. Groundwater-strain coupling before the 1999 M-W 7.6 Taiwan Chi-Chi earthquake. J. Hydrology 524: 378–384, doi: 10.1016/j.jhydrol.2015.03.006.Google Scholar

Chen, J., Verberne, B. A., and Spiers, C. J. 2015a. Interseismic re-strengthening and stabilization of carbonate faults by “non-Dieterich” healing under hydrothermal conditions. Earth Planet. Sci. Lett. 423: 1–12, doi: 10.1016/j.epsl.2015.03.044.Google Scholar

Chen, J. Y., Verberne, B. A., and Spiers, C. J. 2015b. Effects of healing on the seismogenic potential of carbonate fault rocks: Experiments on samples from the Longmenshan Fault, Sichuan, China. J. Geophys. Res.-Solid Earth 120(8): 5479–5506, doi: 10.1002/2015jb012051.Google Scholar

Chen, L., and Talwani, P. 2001. Mechanism of initial seismicity following impoundment of the Monticello Reservoir, South Carolina. Bull. Seismol. Soc. Amer. 91: 94–101.Google Scholar

Chen, T., and Lapusta, N. 2009. Scaling of small repeating earthquakes explained by interaction of seismic and aseismic slip in a rate and state fault model. J. Geophys. Res.-Solid Earth 114, doi: 10.1029/2008jb005749.Google Scholar

Chen, W. P., and Molnar, P. 1983. Focal depths of intracontinental and intraplate earthquakes and their implications for the thermal and mechanical properties of the lithosphere. J. Geophys. Res. 88: 4183–4215.Google Scholar

Chen, X., and Shearer, P. M. 2013. California foreshock sequences suggest aseismic triggering process. Geophys. Res. Lett. 40(11): 2602–2607.Google Scholar

Chen, Y. 1988. Thermal model of oceanic transform faults. J. Geophys. Res. 93: 8839–8851.Google Scholar

Chernak, L. J., and Hirth, G. 2010. Deformation of antigorite serpentinite at high temperature and pressure. Earth Planet. Sci. Lett. 296(1): 23–33.Google Scholar

Chernyshev, S. N., and Dearman, W. R. 1991. Rock Fractures. London: Butterworth-Heinemann Ltd.Google Scholar

Chester, F. M. 1994. Effect of temperature on friction – Constitutive equations and experiments with quartz gouge. J. Geophys. Res. 99: 7247–7261.Google Scholar

Chester, F. M. 1995. A rheologic model for wet crust applied to strike-slip faults. J. Geophys. Res.-Solid Earth 100: 13033–13044.Google Scholar

Chester, F. M., and Chester, J. S. 2000. Stress and deformation along wavy frictional faults. J. Geophys. Res. 105: 23,421–423,430.Google Scholar

Chester, F. M., and Higgs, N. G. 1992. Multimechanism friction constitutive model for ultrafine quartz gouge at hypocentral conditions. J. Geophys. Res.-Solid Earth 97: 1859–1870.Google Scholar

Chester, F. M., and Logan, J. M. 1986. Implications for mechanical properties of brittle faults from observations of the Punchbowl fault zone, California. Pageoph 124: 79–106.Google Scholar

Chester, F. M., Biegel, R. L., and Evans, J. P. 1993. Internal structure and weakening mechanisms of the San-Andreas fault. J. Geophys. Res.-Solid Earth 98: 771–786.Google Scholar

Chester, F. M., Friedman, M., and Logan, J. M. 1985. Foliated cataclasites. Tectonophysics 111: 134–146.Google Scholar

Chester, F. M., Rowe, C. D., Ujiie, K., Kirkpatrick, J. D., Regalla, C., Remitti, F., Moore, J. C., Toy, V. G., Wolfson-Schwehr, M., and Bose, S. 2013. Structure and composition of the plate-boundary slip zone for the 2011 Tohoku-oki earthquake. Science 342: 1208–1211, doi: 10.1126/science.1243719.Google Scholar

Chester, J. S., Chester, F. M., and Kronenberg, A. K. 2005. Fracture surface energy of the Punchbowl fault, San Andreas system. Nature 437(7055): 133–136.Google Scholar

Chiaraluce, L. 2012. Unravelling the complexity of Apenninic extensional fault systems: A review of the 2009 L’Aquila earthquake (Central Apennines, Italy). J. Struct. Geol. 42: 2–18, doi: 10.1016/j.jsg.2012.06.007.Google Scholar

Chiaraluce, L., Chiarabba, C., Collettini, C., Piccinini, D., and Cocco, M. 2007. Architecture and mechanics of an active low-angle normal fault: Alto Tiberina Fault, northern Apennines, Italy. J. Geophys. Res.-Solid Earth 112(B10): doi.org/10.1029/2007JB005015.Google Scholar

Chinnery, M. A. 1961. Deformation of the ground around surface faults. Bull. Seismol. Soc. Am. 51: 355–372.Google Scholar

Chinnery, M. A. 1964. The strength of the earth’s crust under horizontal shear stress. J. Geophys. Res. 69: 2085–2089.Google Scholar

Chlieh, M., Avouac, J.-P., Hjorleifsdottir, V.,et al. 2007. Coseismic slip and afterslip of the great M-w 9.15 Sumatra-Andaman earthquake of 2004. Bull. Seismol. Soc. Am. 97(1): S152–S173, doi: 10.1785/0120050631.Google Scholar

Chlieh, M., Avouac, J.-P., Sieh, K., Natawidjaja, D. H., and Galetzka, J. 2008. Heterogeneous coupling of the Sumatran megathrust constrained by geodetic and paleogeodetic measurements. J. Geophys. Res.-Solid Earth 113(B5): doi.org/10.1029/2007JB004981.Google Scholar

Chlieh, M., Perfettini, H., Tavera, H., et al. 2011. Interseismic coupling and seismic potential along the Central Andes subduction zone. J. Geophys. Res.-Solid Earth 116(B12): doi.org/10.1029/2010JB008166.Google Scholar

Choi, J. H., Edwards, P., Ko, K., and Kim, Y. S. 2016. Definition and classification of fault damage zones: A review and a new methodological approach. Earth-Science Reviews 152: 70–87, doi: 10.1016/j.earscirev.2015.11.006.Google Scholar

Chopra, P. N. 1997. High-temperature transient creep in olivine rocks. Tectonophysics 279(1–4): 93–111, doi: 10.1016/s0040-1951(97)00134–0.Google Scholar

Choy, G. L., and Boatwright, J. L. 1995. Global patterns of radiated energy and apparent stress. J. Geophys. Res.-Solid Earth 100(B9): 18205–18228, doi: 10.1029/95jb01969.Google Scholar

Choy, G. L., and McGarr, A. 2002. Strike-slip earthquakes in the oceanic lithosphere: Observations of exceptionally high apparent stress. Geophys. J. Int. 150(2): 506–523, doi: 10.1046/j.1365-246X.2002.01720.x.Google Scholar

Choy, G. L., McGarr, A., Kirby, S. H., and Boatwright, J. 2006. An overview of the global variability in radiated energy and apparent stress. In Earthquakes: Radiated Energy and the Physics of Faulting, eds. R. Abercrombie, A. McGarr, G. DiToro and H. Kanamori, pp. 43–57, doi: 10.1029/170gm01.Google Scholar

Christensen, D. H., and Ruff, L. 1983. Outer rise earthquakes and seismic coupling. Geophys. Res. Lett. 10: 697–700.Google Scholar

Christie, J. M. 1960. Mylonitic rocks of the Moine thrust zone in the Assynt district, northwest Scotland. Trans. Geol. Soc. Edinburgh 18: 79–93.Google Scholar

Christie-Blick, N., and Biddle, K. T. 1985. Deformation and basin formation along strike-slip faults. In Strike-slip deformation, basin formation, and sedimentation. Soc. Econ. Pal. Miner. Spec. Publ. 37, eds. K. Biddle and N. Christie-Blick. pp. 1–34.Google Scholar

Cicerone, R. D., Ebel, J. E., and Britton, J. 2009. A systematic compilation of earthquake precursors. Tectonophysics 476(3–4): 371–396, doi: 10.1016/j.tecto.2009.06.008.Google Scholar

Cifuentes, I. 1989. The 1960 Chilean Earthquakes. J. Geophys. Res. 94: 665–680, doi: 10.1029/JB094iB01p00665.Google Scholar

Cifuentes, I. L., and Silver, P. G. 1989. Low-frequency source characteristics of the great 1960 Chilean earthquake. J. Geophys. Res. 94: 643–663.Google Scholar

Cirella, A., Piatanesi, A., Cocco, M., Tinti, E., Scognamiglio, L., Michelini, A., Lomax, A., and Boschi, E. 2009. Rupture history of the 2009 L’Aquila (Italy) earthquake from non-linear joint inversion of strong motion and GPS data. Geophys. Res. Lett. 36, doi: 10.1029/2009gl039795.Google Scholar

Cladouhos, T. T., and Allmendinger, R. W. 1993. Finite strain and rotation from fault-slip data. J. Struct. Geol. 15(6): 771–784.Google Scholar

Cladouhos, T. T., and Marrett, R. 1996. Are fault growth and linkage models consistent with power-law distributions of fault lengths? J. Struct. Geol. 18: 281–293.Google Scholar

Cloetingh, S., and Wortel, R. 1986. Stress in the Indo-Australian plate. Tectonophysics 132(1–3): 49–67.Google Scholar

Cocco, M., and Rice, J. R. 2002. Pore pressure and poroelasticity effects in Coulomb stress analysis of earthquake interactions. J. Geophys. Res. 107: ESE 2-1-ESE 2-17, doi: 10.1029/2000JB000138.Google Scholar

Cochard, A., and Madariaga, R. 1996. Complexity of seismicity due to highly rate-dependent friction. J. Geophys. Res. 101: 25321–25336.Google Scholar

Cochran, E. S., Li, Y. G., Shearer, P. M., Barbot, S., Fialko, Y., and Vidale, J. E. 2009. Seismic and geodetic evidence for extensive, long-lived fault damage zones. Geology 37(4): 315–318, doi: 10.1130/g25306a.1.Google Scholar

Cochran, E. S., Vidale, J. E., and Tanaka, S. 2004. Earth tides can trigger shallow thrust fault earthquakes. Science 306(5699): 1164–1166, doi: 10.1126/science.1103961.Google Scholar

Cockerham, R. S., and Eaton, J. P. 1984. The April 24, 1984 Morgan Hill earthquake and its aftershocks. In The 1984 Morgan Hill, California, Earthquake, eds. Bennett, J. and Sherburne, R.. Sacramento, California: Calif. Div. of Mines: Calif. Div. Mines and Geol. Spec. Publ. 68, pp. 209–213.Google Scholar

Collettini, C. 2011. The mechanical paradox of low-angle normal faults: Current understanding and open questions. Tectonophysics 510(3–4): 253–268, doi: 10.1016/j.tecto.2011.07.015.Google Scholar

Collettini, C., and Holdsworth, R. E. 2004. Fault zone weakening and character of slip along low-angle normal faults: Insights from the Zuccale fault, Elba, Italy. J. Geol. Soc. London 161: 1039–1051.Google Scholar

Collettini, C., and Sibson, R. H. 2001. Normal faults, normal friction. Geology 29: 927–930.Google Scholar

Collettini, C., Niemeijer, A., Viti, C., and Marone, C. 2009a. Fault zone fabric and fault weakness. Nature 462(7275): 907–998, doi: 10.1038/nature08585.Google Scholar

Collettini, C., Viti, C., Smith, S. A. F., and Holdsworth, R. E. 2009b. Development of interconnected talc networks and weakening of continental low-angle normal faults. Geology, 37(6): 567–570, doi: 10.1130/g25645a.1.Google Scholar

Collings, R., Lange, D., Rietbrock, A., et al. 2012. Structure and seismogenic properties of the Mentawai segment of the Sumatra subduction zone revealed by local earthquake traveltime tomography. J. Geophys. Res.-Solid Earth 117, doi: 10.1029/2011jb00846Google Scholar

Colombelli, S., Zollo, A., Festa, G., and Picozzi, M. 2014. Evidence for a difference in rupture initiation between small and large earthquakes. Nat. Commun. 5, doi: 10.1038/ncomms4958.Google Scholar

Conneally, J., Childs, C., and Walsh, J. J. 2014. Contrasting origins of breached relay zone geometries. J. Struct. Geol. 58: 59–68.Google Scholar

Contreras, J., Anders, M. H., and Scholz, C. H. 2000. Growth of a normal fault system: Observations from the Lake Malawi basin of the east African rift. J. Struct. Geol. 22: 159–168.Google Scholar

Cook, R. F. 1986. Crack propagation thresholds: A measure of surface energy. J. Mater. Res. 1: 852–860.Google Scholar

Cornell, C. A. 1968. Engineering seismic risk analysis. Bull. Seismol. Soc. Amer. 58: 1583–1606.Google Scholar

Cotton, F., and Coutant, O. 1997. Dynamic stress variations due to shear faults in a plane-layered medium. Geophys. J. Int. 128: 676–688.Google Scholar

Cottrell, A. H. 1953. Dislocations and Plastic Flow in Crystals. Oxford: Clarendon Press.Google Scholar

Coward, M. P., Dewey, J. F., and Hancock, P. L. (eds.). 1987. Continental Extensional Tectonics. London: Blackwell.Google Scholar

Cowie, P. A., and Roberts, G. P. 2001. Constraining slip rates and spacings for active normal faults. J. Struct. Geol. 23(12): 1901–1915, doi: 10.1016/s0191-8141(01)00036–0.Google Scholar

Cowie, P. A., and Scholz, C. H. 1992a. Physical explanation for the displacement length relationship of faults using a post-yield fracture mechanics model. J. Struct. Geol. 14: 1133–1148.Google Scholar