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Volumn 302, Issue 3-4, 1999, Pages 287-296

Restoration of the depression structure at the eastern part of central Kyushu, Japan by means of dislocation modeling

Author keywords

Central kyushu; Dislocation modeling; Half graben; Pull apart basin; Stress field; Subsurface structure

Indexed keywords


EID: 0345677319     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0040-1951(98)00287-X     Document Type: Article
Times cited : (11)

References (15)
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  • 2
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  • 3
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    • Du, Y.1    Aydin, A.2
  • 4
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    • History of basin formation and tectonic evolution at the termination of a large transcurrent fault system: Deformation mode of central Kyushu, Japan
    • Itoh, Y, Takemura, K., Kamata, H., 1998. History of basin formation and tectonic evolution at the termination of a large transcurrent fault system: deformation mode of central Kyushu, Japan. Tectonophysics 284, 135-150.
    • (1998) Tectonophysics , vol.284 , pp. 135-150
    • Itoh, Y.1    Takemura, K.2    Kamata, H.3
  • 5
    • 0024567459 scopus 로고
    • Shishimuta caldera, the buried source of the Yabakei pyroclastic flow in the Hohi volcanic zone, central Kyushu, Japan
    • Kamata, H., 1989a. Shishimuta caldera, the buried source of the Yabakei pyroclastic flow in the Hohi volcanic zone, central Kyushu, Japan. Bull. Volcanol. 51, 41-50.
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    • Kamata, H.1
  • 6
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    • Volcanic and structural history of the Hohi volcanic zone, central Kyushu, Japan
    • Kamata, H., 1989b. Volcanic and structural history of the Hohi volcanic zone, central Kyushu, Japan. Bull. Volcanol. 51, 315-332.
    • (1989) Bull. Volcanol. , vol.51 , pp. 315-332
    • Kamata, H.1
  • 7
    • 0041976152 scopus 로고
    • Right-lateral movement of the oita-kumamoto tectonic line as a western extension of the median tectonic line, originated from rightward, oblique subduction of the Philippine Sea plate
    • in Japanese with English abstract
    • Kamata, H., 1992. Right-lateral movement of the Oita-Kumamoto Tectonic Line as a western extension of the Median Tectonic Line, originated from rightward, oblique subduction of the Philippine Sea plate. Mem. Geol. Soc. Jpn. 40, 50-63 (in Japanese with English abstract).
    • (1992) Mem. Geol. Soc. Jpn. , vol.40 , pp. 50-63
    • Kamata, H.1
  • 8
    • 0000661230 scopus 로고
    • The Hohi volcanic zone as a volcano-tectonic depression and its formation tectonics Three tectonic events caused by subduction of the Philippine Sea plate under the junction of the Southwest Japan Arc and Ryukyu Arc
    • in Japanese with English abstract
    • Kamata, H., Kodama, K., 1993. The Hohi volcanic zone as a volcano-tectonic depression and its formation tectonics Three tectonic events caused by subduction of the Philippine Sea plate under the junction of the Southwest Japan Arc and Ryukyu Arc. Mem. Geol. Soc. Jpn. 41, 129-148 (in Japanese with English abstract).
    • (1993) Mem. Geol. Soc. Jpn. , vol.41 , pp. 129-148
    • Kamata, H.1    Kodama, K.2
  • 9
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    • Mechanics of graben formation in crustal rocks: A finite element analysis
    • Melosh, H.J., Williams Jr., C.A., 1989. Mechanics of graben formation in crustal rocks: a finite element analysis. J. Geophys. Res. 94, 13961-13973.
    • (1989) J. Geophys. Res. , vol.94 , pp. 13961-13973
    • Melosh, H.J.1    Williams Jr., C.A.2
  • 10
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    • Regional exploration of geothermal fluid circulation system, Tsurumidake area
    • in Japanese
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    • (1990) Natl. Geotherm. Resour. Explor. Proj. (3rd Phase)
  • 11
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  • 12
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  • 13
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    • Basement structure of the Hohi area, Central Kyushu, Japan
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    • Sasada, M., 1984. Basement structure of the Hohi area, Central Kyushu, Japan. J. Jpn. Geotherm. Energy Assoc. 21, 1-11 (in Japanese).
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  • 14
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.