Results 171 to 180 of about 3,084 (214)

Gravity-induced seismicity modulation on planetary bodies and their natural satellites. [PDF]

Sci Rep
Senapati B, Kundu B, Jha B, Jin S.
europepmc   +1 more source

Perturbation-induced granular fluidization as a model for remote earthquake triggering. [PDF]

Sci Adv
Farain K, Bonn D.
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Velocity, Porosity, and Pore-Fluid Loss from the Nankai Subduction Zone Accretionary Prism

, 1993
R.D. Hyndman, G.F. Moore, K. Moran
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Moderate heating renders 7.8-million-year-old sedimentary organic matter bioavailable. [PDF]

Sci Adv
Gan S, Heuer VB, Schmidt F, Wörmer L, Wang F, Adhikari RR, Hatcher P, Pearson A, Hinrichs KU.   +8 more
europepmc   +1 more source

Crustal deformation at the Nankai subduction zone, southwest Japan, derived from GPS measurements

Crustal deformation at the Nankai subduction zone, southwest Japan, derived from GPS measurements
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Splay Fault Branching Along the Nankai Subduction Zone

Science, 2002
Seismic reflection profiles reveal steeply landward–dipping splay faults in the rupture area of the magnitude (M) 8.1 Tonankai earthquake in the Nankai subduction zone. These splay faults branch upward from the plate-boundary interface (that is, the subduction zone) at a depth of ∼10 kilometers, ∼50 to 55 kilometers landward of the trough axis ...
Jin-Oh, Park, Tetsuro, Tsuru, Shuichi, Kodaira, Phil R, Cummins, Yoshiyuki, Kaneda   +4 more
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Slow Earthquakes Linked Along Dip in the Nankai Subduction Zone

Science, 2010
Three types of temporally linked slow earthquakes may limit nearby buildup of stress.
Hitoshi, Hirose, Youichi, Asano, Kazushige, Obara, Takeshi, Kimura, Takanori, Matsuzawa, Sachiko, Tanaka, Takuto, Maeda   +6 more
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Interseismic deformation at the Nankai Trough, Japan, subduction zone

Journal of Geophysical Research: Solid Earth, 1992
Uplift along the coast of southwestern Japan following the 1944 Tonankai (Ms = 8.0) and 1946 Nankaido (Ms = 8.2) earthquakes has been inferred from the 1950–1985 tide gage records. Although uplift rates vary with geographic position, the temporal dependence at each site can be described as the superposition of an exponentially decaying (time constant ...
J. C. Savage, W. Thatcher
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A low-velocity zone with weak reflectivity along the Nankai subduction zone

Geology, 2010
Three-dimensional seismic reflection data reveal the presence of a low seismic velocity zone (LVZ) with weak reflectivity character along the Nankai accretionary prism. This LVZ is intercalated between an upper, offscraped layer and a lower, underthrusting layer in the outer accretionary wedge.
Jin-Oh Park, Gou Fujie, Lalith Wijerathne, Takane Hori, Shuichi Kodaira, Yoshio Fukao, Gregory F. Moore, Nathan L. Bangs, Shin'ichi Kuramoto, Asahiko Taira   +9 more
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