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Volumn 174, Issue 1, 2008, Pages 331-335

Long-term slow slip events are not necessarily caused by high pore fluid pressure at the plate interface: An implication from two-dimensional model calculations

Author keywords

Computational seismology; Hydrogeophysics; Numerical approximations and analysis; Rheology and friction of fault zones; Seismic cycle; Subduction zone processes

Indexed keywords

FAULT SLIP; FAULT ZONE; FRICTION; NUMERICAL MODEL; PORE PRESSURE; RHEOLOGY; SEISMOLOGY; SUBDUCTION ZONE;

EID: 45249099550     PISSN: 0956540X     EISSN: 1365246X     Source Type: Journal    
DOI: 10.1111/j.1365-246X.2008.03832.x     Document Type: Article
Times cited : (8)

References (25)
  • 1
    • 0032503213 scopus 로고    scopus 로고
    • Quantitative measure of the variation in fault rheology due to fluid-rock interactions
    • Blanpied, M.L., Marone, C.J., Lockner, D.A., Byerlee, J.D. & King, D.P., 1998. Quantitative measure of the variation in fault rheology due to fluid-rock interactions, J. geophys. Res., 103 (B5), 9691-9712.
    • (1998) J. Geophys. Res., , vol.103 , Issue.B5 , pp. 9691-9712
    • Blanpied, M.L.1    Marone, C.J.2    Lockner, D.A.3    Byerlee, J.D.4    King, D.P.5
  • 2
    • 84986409721 scopus 로고
    • Pore pressure and oceanic crustal seismic structure
    • Christensen, N.I., 1984. Pore pressure and oceanic crustal seismic structure, Geophys. J. R. astr. Soc., 79, 411-423.
    • (1984) Geophys. J. R. Astr. Soc. , vol.79 , pp. 411-423
    • Christensen, N.I.1
  • 3
    • 77950792882 scopus 로고
    • Modeling of rock friction 1. Experimental results and constitutive equations
    • Dieterich, J.H., 1979. Modeling of rock friction 1. Experimental results and constitutive equations, J. geophys. Res., 84 (B5), 2161-2168.
    • (1979) J. Geophys. Res. , vol.84 , Issue.B5 , pp. 2161-2168
    • Dieterich, J.H.1
  • 4
    • 0035947206 scopus 로고    scopus 로고
    • A silent slip event on the deeper Cascadia subduction interface
    • Dragert, H., Wang, K. & James, T.S., 2001. A silent slip event on the deeper Cascadia subduction interface, Science, 292, 1525-1528.
    • (2001) Science , vol.292 , pp. 1525-1528
    • Dragert, H.1    Wang, K.2    James, T.S.3
  • 5
    • 0242281000 scopus 로고    scopus 로고
    • Thermal models of flat subduction and the rupture zone of great subduction earthquakes
    • doi 10.1029/2001JB000787
    • Gutscher, M.A. & Peacock, S.M., 2003. Thermal models of flat subduction and the rupture zone of great subduction earthquakes, J, geophys. Res., 108 (B1), doi 10.1029/2001JB000787.
    • (2003) J, Geophys. Res. , vol.108 , Issue.B1
    • Gutscher, M.A.1    Peacock, S.M.2
  • 7
    • 33845612688 scopus 로고    scopus 로고
    • Short-term slow slip and correlated tremor episodes in the Tokai region, central Japan
    • doi 10.1029/2006GL026579
    • Hirose, H. & Obara, K., 2006. Short-term slow slip and correlated tremor episodes in the Tokai region, central Japan, Geophys. Res. Lett., 33 (L17311), doi 10.1029/2006GL026579.
    • (2006) Geophys. Res. Lett. , vol.33 , Issue.L17311
    • Hirose, H.1    Obara, K.2
  • 8
    • 0033226715 scopus 로고    scopus 로고
    • A slow thrust slip event following the two 1996 Hyuganada earthquakes beneath the Bungo Channel, southwest Japan
    • Hirose, H., Hirahara, K., Kimata, F., Fujii, N. & Miyazaki, S., 1999. A slow thrust slip event following the two 1996 Hyuganada earthquakes beneath the Bungo Channel, southwest Japan, Geophys. Res. Lett., 26 (21), 3237-3240.
    • (1999) Geophys. Res. Lett. , vol.26 , Issue.21 , pp. 3237-3240
    • Hirose, H.1    Hirahara, K.2    Kimata, F.3    Fujii, N.4    Miyazaki, S.5
  • 9
    • 0031399423 scopus 로고    scopus 로고
    • The seismogenic zone of subduction thrust faults
    • Hyndman, R.D., Yamano, M. & Oleskevich, D.A., 1997. The seismogenic zone of subduction thrust faults, The Island Arc, 1997 (6), 244-260.
    • (1997) The Island Arc , vol.1997 , Issue.6 , pp. 244-260
    • Hyndman, R.D.1    Yamano, M.2    Oleskevich, D.A.3
  • 10
    • 0030702804 scopus 로고    scopus 로고
    • A numerical study on seismic coupling along subduction zones using a laboratory-derived friction law
    • Kato, N. & Hirasawa, T., 1997. A numerical study on seismic coupling along subduction zones using a laboratory-derived friction law, Phys. Earth planet. Inter., 102, 51-68.
    • (1997) Phys. Earth Planet. Inter. , vol.102 , pp. 51-68
    • Kato, N.1    Hirasawa, T.2
  • 11
    • 2542638085 scopus 로고    scopus 로고
    • High pore pressure may cause silent slip in the Nankai Trough
    • Kodaira, S., Iidaka, T., Kato, A., Park, J., Iwasaki, T. & Kaneda, Y., 2004. High pore pressure may cause silent slip in the Nankai Trough, Science, 304, 1295-1298.
    • (2004) Science , vol.304 , pp. 1295-1298
    • Kodaira, S.1    Iidaka, T.2    Kato, A.3    Park, J.4    Iwasaki, T.5    Kaneda, Y.6
  • 12
    • 0042812314 scopus 로고    scopus 로고
    • Nucleation and early seismic propagation of small and large events in a crustal earthquake model
    • doi 10.1029/2001JB000793
    • Lapusta, N. & Rice, J.R., 2003. Nucleation and early seismic propagation of small and large events in a crustal earthquake model, J. geophys. Res., 108 (B4), doi 10.1029/2001JB000793.
    • (2003) J. Geophys. Res. , vol.108 , Issue.B4
    • Lapusta, N.1    Rice, J.R.2
  • 13
    • 26844456424 scopus 로고    scopus 로고
    • Aseismic slip transients emerge spontaneously in three-dimensinal rate and state modeling of subduction earthquake sequences
    • doi 10.1029/2004JB003424
    • Liu, Y. & Rice, J.R., 2005. Aseismic slip transients emerge spontaneously in three-dimensinal rate and state modeling of subduction earthquake sequences, J. geophys. Res., 110 (B8), doi 10.1029/ 2004JB003424.
    • (2005) J. Geophys. Res. , vol.110 , Issue.B8
    • Liu, Y.1    Rice, J.R.2
  • 14
    • 16644376328 scopus 로고    scopus 로고
    • Episodic slow slip events accompanied by non-volcanic tremors in southwest Japan subduction zone
    • doi 10.1029/2004GL020848
    • Obara, K., Hirose, H., Yamamizu, F. & Kasahara, K., 2004. Episodic slow slip events accompanied by non-volcanic tremors in southwest Japan subduction zone, Geophys. Res. Lett., 31 (L23602), doi 10.1029/ 2004GL020848.
    • (2004) Geophys. Res. Lett. , vol.31 , Issue.L23602
    • Obara, K.1    Hirose, H.2    Yamamizu, F.3    Kasahara, K.4
  • 15
    • 33745184048 scopus 로고    scopus 로고
    • A large slow slip event and the depth of the seismogenic zone in the south central Alaska subduction zone
    • Ohta, Y., Freymueller, J.T., Hreinsdottir, S. & Suito, H., 2006. A large slow slip event and the depth of the seismogenic zone in the south central Alaska subduction zone, Earth planet. Sci. Lett., 247, 108-116.
    • (2006) Earth Planet. Sci. Lett. , vol.247 , pp. 108-116
    • Ohta, Y.1    Freymueller, J.T.2    Hreinsdottir, S.3    Suito, H.4
  • 18
    • 0026476468 scopus 로고
    • Static deformation of a uniform half-space due to a long dip-slip fault
    • Rani, S. & Singh, S.J., 1992. Static deformation of a uniform half-space due to a long dip-slip fault, Geophys. J. Int., 109, 469-476.
    • (1992) Geophys. J. Int. , vol.109 , pp. 469-476
    • Rani, S.1    Singh, S.J.2
  • 19
    • 0027427011 scopus 로고
    • Spatio-temporal complexity of slip on a fault
    • Rice, J.R., 1993. Spatio-temporal complexity of slip on a fault, J. geophys. Res., 98 (B6), 9885-9907.
    • (1993) J. Geophys. Res. , vol.98 , Issue.B6 , pp. 9885-9907
    • Rice, J.R.1
  • 20
    • 0020968914 scopus 로고
    • Slip instability and state variable friction laws
    • Ruina, A., 1983. Slip instability and state variable friction laws, J. geophys. Res., 88 (B12), 10359-10370.
    • (1983) J. Geophys. Res. , vol.88 , Issue.B12 , pp. 10359-10370
    • Ruina, A.1
  • 21
    • 35248828009 scopus 로고    scopus 로고
    • Modelling of short-interval silent slip events in deeper subduction interfaces considering the frictional properties at the unstable-stable transition regime
    • Shibazaki, B. & Shimamoto, T., 2007. Modelling of short-interval silent slip events in deeper subduction interfaces considering the frictional properties at the unstable-stable transition regime, Geophys. J. Int., 171, 191-205.
    • (2007) Geophys. J. Int. , vol.171 , pp. 191-205
    • Shibazaki, B.1    Shimamoto, T.2
  • 22
    • 0242581652 scopus 로고    scopus 로고
    • Reaction-enhanced permeability during serpentinite dehydration
    • Tenthorey, E. & Cox, S.F., 2003. Reaction-enhanced permeability during serpentinite dehydration, Geology, 31 (10), 921-924.
    • (2003) Geology , vol.31 , Issue.10 , pp. 921-924
    • Tenthorey, E.1    Cox, S.F.2
  • 23
    • 33746407667 scopus 로고    scopus 로고
    • A large slow slip event on the central Hikurangi subduction interface beneath the Manawatu region, North Islands, New Zealand
    • doi 10.1029/2006GL026009
    • Wallace, L.M. & Beavan, J., 2006. A large slow slip event on the central Hikurangi subduction interface beneath the Manawatu region, North Islands, New Zealand, Geophys. Res. Lett., 33, L11301, doi 10.1029/2006GL026009.
    • (2006) Geophys. Res. Lett. , vol.33
    • Wallace, L.M.1    Beavan, J.2
  • 24
    • 0033947813 scopus 로고    scopus 로고
    • Stress-strain 'paradox', plate coupling, and forearc seismicity at the Cascadia and Nankai subduction zones
    • Wang, K., 2000. Stress-strain 'paradox', plate coupling, and forearc seismicity at the Cascadia and Nankai subduction zones, Tectonophysics, 319, 321-338.
    • (2000) Tectonophysics , vol.319 , pp. 321-338
    • Wang, K.1
  • 25
    • 35248851079 scopus 로고    scopus 로고
    • Temperature distribution of the upper surface of the subducted Philippine Sea Plate along the Nankai Trough, southwest Japan, from a three-dimensional subduction model: Relation to large interplate and low-frequency earthquakes
    • Yoshioka, S. & Murakami, K., 2007. Temperature distribution of the upper surface of the subducted Philippine Sea Plate along the Nankai Trough, southwest Japan, from a three-dimensional subduction model: relation to large interplate and low-frequency earthquakes, Geophys. J. Int., 171, 302-315.
    • (2007) Geophys. J. Int. , vol.171 , pp. 302-315
    • Yoshioka, S.1    Murakami, K.2


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