Formation and shortening deformation of a back-arc rift basin revealed by deep seismic profiling, central Japan

Hiroshi Sato, Takaya Iwasaki, Shinji Kawasaki, Yasutaka Ikeda, Nobuhisa Matsuta, Tetsuya Takeda, Naoshi Hirata, Taku Kawanaka

Research output: Contribution to journalArticle

37 Citations (Scopus)

Abstract

The northern Fossa Magna (NFM) basin is a Miocene rift system produced in the final stages of the opening of the Sea of Japan. It divides the major structure of Japan into two regions, with north-trending geological structures to the NE of the basin and EW trending structures to the west of the basin. The Itoigawa-Shizuoka Tectonic Line (ISTL) bounds the western part of the northern Fossa Magna and forms an active fault system that displays one of the largest slip rates (4-9 mm/year) in the Japanese islands. Deep seismic reflection and refraction/wide-angle reflection profiling were undertaken in 2002 across the northern part of ISTL in order to delineate structures in the crust, and the deep geometry of the active fault systems. The seismic images are interpreted based on the pattern of reflectors, the surface geology and velocities derived from refraction analysis. The 68-km-long seismic section suggests that the Miocene NFM basin was formed by an east dipping normal fault with a shallow flat segment to 6 km depth and a deeper ramp penetrating to 15 km depth. This low-angle normal fault originated as a comparatively shallow brittle/ductile detachment in a high thermal regime present in the Miocene. The NFM basin was filled by a thick (>6 km) accumulation of sediments. Shortening since the late Neogene is accommodated along NS to NE-SE trending thrust faults that previously accommodated extension and produce fault-related folds on their hanging wall. Based on our balanced geologic cross-section, the total amount of Miocene extension is ca. 42 km and the total amount of late Neogene to Quaternary shortening is ca. 23 km.

Original languageEnglish
Pages (from-to)47-58
Number of pages12
JournalTectonophysics
Volume388
Issue number1-4 SPEC. ISS.
DOIs
Publication statusPublished - Sep 13 2004
Externally publishedYes

Fingerprint

Japan
arcs
Miocene
basin
active fault
normal fault
Neogene
refraction
tectonics
Sea of Japan
slip rate
thermal regime
seismic refraction
hanging wall
display devices
geology
thrust fault
ramps
dipping
geological structure

Keywords

  • Basin inversion
  • Deep seismic profiling
  • Fossa Magna
  • Itoigawa-Shizuoka Tectonic Line
  • Japan
  • Low-angle normal fault

ASJC Scopus subject areas

  • Earth-Surface Processes
  • Geophysics

Cite this

Formation and shortening deformation of a back-arc rift basin revealed by deep seismic profiling, central Japan. / Sato, Hiroshi; Iwasaki, Takaya; Kawasaki, Shinji; Ikeda, Yasutaka; Matsuta, Nobuhisa; Takeda, Tetsuya; Hirata, Naoshi; Kawanaka, Taku.

In: Tectonophysics, Vol. 388, No. 1-4 SPEC. ISS., 13.09.2004, p. 47-58.

Research output: Contribution to journalArticle

Sato, H, Iwasaki, T, Kawasaki, S, Ikeda, Y, Matsuta, N, Takeda, T, Hirata, N & Kawanaka, T 2004, 'Formation and shortening deformation of a back-arc rift basin revealed by deep seismic profiling, central Japan', Tectonophysics, vol. 388, no. 1-4 SPEC. ISS., pp. 47-58. https://doi.org/10.1016/j.tecto.2004.07.004
Sato, Hiroshi ; Iwasaki, Takaya ; Kawasaki, Shinji ; Ikeda, Yasutaka ; Matsuta, Nobuhisa ; Takeda, Tetsuya ; Hirata, Naoshi ; Kawanaka, Taku. / Formation and shortening deformation of a back-arc rift basin revealed by deep seismic profiling, central Japan. In: Tectonophysics. 2004 ; Vol. 388, No. 1-4 SPEC. ISS. pp. 47-58.
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AU - Sato, Hiroshi

AU - Iwasaki, Takaya

AU - Kawasaki, Shinji

AU - Ikeda, Yasutaka

AU - Matsuta, Nobuhisa

AU - Takeda, Tetsuya

AU - Hirata, Naoshi

AU - Kawanaka, Taku

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