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Volumn 102, Issue B9, 1997, Pages 20539-20550

Three-dimensional dislocation model for great earthquakes of the Cascadia subduction zone

Author keywords

[No Author keywords available]

Indexed keywords

DISLOCATION MODEL; EARTHQUAKE; SUBDUCTION ZONE; SURFACE DEFORMATION;

EID: 0031422067     PISSN: 21699313     EISSN: 21699356     Source Type: Journal    
DOI: None     Document Type: Article
Times cited : (143)

References (10)
  • 1
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    • Paleoseismicity of the cascadia subduction zone: Evidence from turbidites off the Oregon-Washington margin
    • Adams, J.,Paleoseismicity of the Cascadia subduction zone: Evidence from turbidites off the Oregon-Washington margin, Tectonics, 9, 569-583, 1990.
    • (1990) Tectonics , vol.9 , pp. 569-583
    • Adams, J.1
  • 2
    • 0018480364 scopus 로고
    • Geodetic evidence for aseismic subduction of the Juan de Fuca plate
    • Ando, M.,and E.I. Balazs, Geodetic evidence for aseismic subduction of the Juan de Fuca plate, J. Geophys. Res.,84, 3023-3028, 1979.
    • (1979) J. Geophys. Res. , vol.84 , pp. 3023-3028
    • Ando, M.1    Balazs, E.I.2
  • 3
    • 0001815399 scopus 로고
    • Consensus about past great earthquakes at the Cascadia subduction zone
    • Atwater, B.F.,et al., Consensus about past great earthquakes at the Cascadia subduction zone, Earthquake Spectra, 11, 1-18, 1995.
    • (1995) Earthquake Spectra , vol.11 , pp. 1-18
    • Atwater, B.F.1
  • 4
    • 0028806959 scopus 로고
    • Upper mantle structure of the northern Cascadia subduction zone
    • Bostock, M.G.,and J.C. VanDecar, Upper mantle structure of the northern Cascadia subduction zone, Can. J. Earth Sci.,32, 1-12, 1995.
    • (1995) Can. J. Earth Sci. , vol.32 , pp. 1-12
    • Bostock, M.G.1    Vandecar, J.C.2
  • 5
    • 0024255280 scopus 로고
    • Loci and maximum size of thrust earthquakes and the mechanics of the shallow region of subduction zones
    • Byrne, D.E., D.M. Davis, and L.R. Sykes, Loci and maximum size of thrust earthquakes and the mechanics of the shallow region of subduction zones, Tectonics, 7, 833-857, 1988.
    • (1988) Tectonics , vol.7 , pp. 833-857
    • Byrne, D.E.1    Davis, D.M.2    Sykes, L.R.3
  • 6
    • 0029476145 scopus 로고
    • A review of receiver function studies in the southern Canadian Cordillera
    • Cassidy, J.,A review of receiver function studies in the southern Canadian Cordillera, Can. J. Earth. Sci.,32, 938-951, 1995.
    • (1995) Can. J. Earth. Sci. , vol.32 , pp. 938-951
    • Cassidy, J.1
  • 7
    • 0027385846 scopus 로고
    • S-wave velocity structure of the northern Cascadia subduction zone
    • Cassidy, J.,and R.M. Ellis, S-wave velocity structure of the northern Cascadia subduction zone, J. Geophys. Res.,98, 4407-4421, 1993.
    • (1993) J. Geophys. Res. , vol.98 , pp. 4407-4421
    • Cassidy, J.1    Ellis, R.M.2
  • 8
    • 0028328029 scopus 로고
    • Evidence for a large earthquake and tsunami 100-400 years ago on western Vancouver Island, British Columbia
    • Clague, J.J.,and P.T. Bobrowsky, Evidence for a large earthquake and tsunami 100-400 years ago on western Vancouver Island, British Columbia, Quat. Res.,41, 176-184, 1994.
    • (1994) Quat. Res. , vol.41 , pp. 176-184
    • Clague, J.J.1    Bobrowsky, P.T.2
  • 9
    • 0019999682 scopus 로고
    • Late Quaternary sea levels and crustal movements, coastal British Columbia
    • Clague, J.J., J.R. Harper, R.J. Hebda, and D.E. Howes, Late Quaternary sea levels and crustal movements, coastal British Columbia, Can. J. Earth Sci.,19, 597-618, 1982.
    • (1982) Can. J. Earth Sci. , vol.19 , pp. 597-618
    • Clague, J.J.1    Harper, J.R.2    Hebda, R.J.3    Howes, D.E.4
  • 10
    • 0023522904 scopus 로고
    • Slab geometry of the Cascadia subduction zone beneath Washington from earthquake hypocenters and teleseismic converted waves
    • Crosson, R.S.,and T.J. Owens, Slab geometry of the Cascadia subduction zone beneath Washington from earthquake hypocenters and teleseismic converted waves, Geophys. Res. Lett.,14, 824-827, 1987.
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    • Crosson, R.S.1    Owens, T.J.2


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.