Proc. IODP, 314/315/316, Data report: frictional healing and compressibility of sheared sediment from fault zones, Sites C0004 and C0007

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Chapter contents Abstract Introduction Sample descriptions Site C0004 Site C0007 Experimental methods Results Frictional healing Compaction Compressibility Acknowledgments References Figures F1. Map of the Nankai area. F2. Profile of accretionary prism. F3. Biaxial deformation apparatus and pressure vessel. F4. Stress-displacement curves, Site C0004. F5. Stress-displacement curves, Site C0007. F6. Slide-hold-slide sequence. F7. Normal stress steps and change in sample layer thickness. F8. Frictional healing data, Site C0004. F9. Frictional healing data, Site C0004. F10. Compaction data, Site C0004. F11. Compaction data, Site C0007. F12. Results of normal stress steps, Site C0004. Tables T1. Samples tested and experiment parameters. T2. Slide-hold-slide parameters, Site C0004. T3. Slide-hold-slide parameters, Site C0007. T4. Curve fits for frictional healing and compaction. T5. Normal stress step parameters. T6. Compressibility. PDF file			Previous \| Next doi:10.2204/iodp.proc.314315316.219.2012 References Biot, M.A., 1941. General theory of three-dimensional consolidation. J. Appl. Phys., 12(2):155–164. doi:10.1063/1.1712886 Dieterich, J.H., 1972. Time-dependent friction in rocks. J. Geophys. Res., [Solid Earth], 77(20):3690–3697. doi:10.1029/JB077i020p03690 Expedition 316 Scientists, 2009a. Expedition 316 Site C0004. In Kinoshita, M., Tobin, H., Ashi, J., Kimura, G., Lallemant, S., Screaton, E.J., Curewitz, D., Masago, H., Moe, K.T., and the Expedition 314/315/316 Scientists, Proc. IODP, 314/315/316: Washington, DC (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.314315316.133.2009 Expedition 316 Scientists, 2009b. Expedition 316 Site C0007. In Kinoshita, M., Tobin, H., Ashi, J., Kimura, G., Lallemant, S., Screaton, E.J., Curewitz, D., Masago, H., Moe, K.T., and the Expedition 314/315/316 Scientists, Proc. IODP, 314/315/316: Washington, DC (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.314315316.135.2009 Gercek, H., 2007. Poisson’s ratio values for rocks. Int. J. Rock Mech. Min. Sci., 44(1):1–13. doi:10.1016/j.ijrmms.2006.04.011 Handin, J., 1969. On the Coulomb-Mohr failure criterion. J. Geophys. Res., [Solid Earth], 74(22):5343–5348. doi:10.1029/JB074i022p05343 Ikari, M.J., and Saffer, D.M., 2011. Comparison of frictional strength and velocity dependence between fault zones in the Nankai accretionary complex. Geochem., Geophys., Geosyst., 12:Q0AD11. doi:10.1029/2010GC003442 Ikari, M.J., Saffer, D.M., and Marone, C., 2009. Frictional and hydrologic properties of a major splay fault system, Nankai subduction zone. Geophys. Res. Lett., 36(20):L20313. doi:10.1029/2009GL040009 Jaeger, J.C., Cook, N.G.W., and Zimmerman, R., 2007. Fundamentals of Rock Mechanics (4th ed.): Malden, MA (Blackwell Publ.). Kimura, G., Screaton, E.J., Curewitz, D., and the Expedition 316 Scientists, 2008. NanTroSEIZE Stage 1A: NanTroSEIZE shallow megasplay and frontal thrusts. IODP Prel. Rept., 316. doi:10.2204/iodp.pr.316.2008 Marone, C., 1998. The effect of loading rate on static friction and the rate of fault healing during the earthquake cycle. Nature (London, U. K.), 391(6662):69–72. doi:10.1038/34157 Moore, J.C., and Saffer, D., 2001. Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: an effect of diagenetic to low-grade metamorphic processes and increasing effective stress. Geology, 29(2):183–186. doi:10.1130/0091-7613(2001)029<0183:ULOTSZ>2.0.CO;2 Shipboard Scientific Party, 2001. Leg 190 summary. In Moore, G.F., Taira, A., Klaus, A., et al., Proc. ODP, Init. Repts., 190: College Station, TX (Ocean Drilling Program), 1–87. doi:10.2973/odp.proc.ir.190.101.2001 Top of page \| Previous \| Next

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