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Satoshi MATSUMOTO

Biographic Data

ID9510719
NAMESatoshi MATSUMOTO
GIVEN NAMESSatoshi
FAMILY NAMEMATSUMOTO
SIGNATUREMATSUMOTO S
AFFILIATIONSKyushu University
ORCID0000-0001-7925-801X
VERIFIEDYes
TOTAL WORKS2
TOTAL CITATIONS0
WORKS AS AUTHOR2
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2020
LATEST PUBLICATION YEAR2020
H-INDEX0
  • Hyper Dense Seismic Observation for Investigation on Fault Zone Development

    Open Access•Satoshi MATSUMOTO, Yoshihisa IIO et al.•ARTICLE•Journal of Geography (Chigaku…•2020

    One important factor controlling crustal strength is fault zone development. A fault can mature through multiple stages where small faults are generated by rupturing homogeneous media, and are partially connected each other, with large deformations locally concentrated along a major fault. Fault geometry, stress field, and seismic activity, which are detectable with seismic observations, may depend on the stage of fault evolution. At the same tim…

  • The Quaternary Tectonics of Central Kyushu and the 2016 Kumamoto Earthquake

    Open Access•Kiyokazu OOHASHI, Makoto Otsubo et al.•ARTICLE•Journal of Geography (Chigaku…•2020

    The 2016 Kumamoto earthquake occurred in the tectonically complex central Kyushu area where several forcing factors such as the subducting Philippine Sea plate, the Median Tectonic Line and the Nankai forearc sliver, the spreading Okinawa trough, and the migrating volcanic front are involved. Neogene–Quaternary tectonics of central Kyushu are revisited by integrating geological, seismological, and geodetical approaches. Deformation histories of t…

No prominent works on this page.

  • Hyper Dense Seismic Observation for Investigation on Fault Zone Development

    Open Access•Satoshi MATSUMOTO, Yoshihisa IIO et al.•ARTICLE•Journal of Geography (Chigaku…•2020

    One important factor controlling crustal strength is fault zone development. A fault can mature through multiple stages where small faults are generated by rupturing homogeneous media, and are partially connected each other, with large deformations locally concentrated along a major fault. Fault geometry, stress field, and seismic activity, which are detectable with seismic observations, may depend on the stage of fault evolution. At the same tim…

  • The Quaternary Tectonics of Central Kyushu and the 2016 Kumamoto Earthquake

    Open Access•Kiyokazu OOHASHI, Makoto Otsubo et al.•ARTICLE•Journal of Geography (Chigaku…•2020

    The 2016 Kumamoto earthquake occurred in the tectonically complex central Kyushu area where several forcing factors such as the subducting Philippine Sea plate, the Median Tectonic Line and the Nankai forearc sliver, the spreading Okinawa trough, and the migrating volcanic front are involved. Neogene–Quaternary tectonics of central Kyushu are revisited by integrating geological, seismological, and geodetical approaches. Deformation histories of t…

earthquake and tectonic studies (2 works) · Fault (geology) (2 works) · Geological and Geochemical Analysis (2 works) · Geology (2 works) · Geology (2 works) · Seismology (2 works) · Crust (1 work) · Forearc (1 work) · Geology and Paleoclimatology Research (1 work) · Geophysics (1 work)

Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae