Pore pressure in the nankai trough off the kii peninsula, Japan

Insight into evolution of mega-splay fault

Takeshi Tsuji, Rie Kamei, R. Gerhard Pratt

研究成果: 会議への寄与タイプ論文

抄録

We used a theoretical method for predicting effective stress and pore pressure based on rock physics models. To predict the pore pressure around the seismogenic mega-splay fault in the Nankai Trough, we used elastic velocities of discrete samples in addition to the drilling data. First, we developed a theoretical relationship between elastic velocity and effective stress from the crack aspect ratio spectrum estimated from laboratory and well-log data, by using differential effective medium (DEM) theory. Then we estimated in situ effective stress within the accretionary prism by iteratively fitting the theoretically calculated velocities (i.e., elastic moduli) to the seismic velocities derived from waveform tomography. Pore pressure is then obtained as the difference between the effective stress and the confining stress. Using this method, we can use information of velocity-pressure relationship of discrete samples in the pore pressure prediction. Because elastic properties of the deep mega-splay fault are not available from the drilling data, we used properties of outcrop discrete samples acquired at ancient mega-splay fault. Our results suggest an abnormally high pore pressure zone at the footwall side of the mega-splay fault. The abnormal pore pressure zone extends from the mega-splay fault to the seaward accretionary prism. This indicates that the rupture may have propagated from the mega-splay fault to the seaward region, and may have caused large tsunami (close to the trough) as in the case of the 2011 Tohoku earthquake. We further identify ancient mega-splay faults at the landward side of the active mega-splay fault. From the fault system revealed in this study, we interpret that the mega-splay faults are sequentially developed.

元の言語英語
出版物ステータス出版済み - 1 1 2012
イベント18th Formation Evaluation Symposium of Japan 2012 - Chiba, 日本
継続期間: 9 27 20129 28 2012

その他

その他18th Formation Evaluation Symposium of Japan 2012
日本
Chiba
期間9/27/129/28/12

Fingerprint

Pore pressure
pore pressure
trough
effective stress
Prisms
Drilling
accretionary prism
Tsunamis
Information use
Tomography
drilling
Aspect ratio
Earthquakes
Tohoku earthquake 2011
Physics
Elastic moduli
Rocks
Cracks
elastic property
elastic modulus

All Science Journal Classification (ASJC) codes

  • Economic Geology
  • Geochemistry and Petrology
  • Geology
  • Geotechnical Engineering and Engineering Geology
  • Energy Engineering and Power Technology

これを引用

Tsuji, T., Kamei, R., & Pratt, R. G. (2012). Pore pressure in the nankai trough off the kii peninsula, Japan: Insight into evolution of mega-splay fault. 論文発表場所 18th Formation Evaluation Symposium of Japan 2012, Chiba, 日本.

Pore pressure in the nankai trough off the kii peninsula, Japan : Insight into evolution of mega-splay fault. / Tsuji, Takeshi; Kamei, Rie; Pratt, R. Gerhard.

2012. 論文発表場所 18th Formation Evaluation Symposium of Japan 2012, Chiba, 日本.

研究成果: 会議への寄与タイプ論文

Tsuji, T, Kamei, R & Pratt, RG 2012, 'Pore pressure in the nankai trough off the kii peninsula, Japan: Insight into evolution of mega-splay fault' 論文発表場所 18th Formation Evaluation Symposium of Japan 2012, Chiba, 日本, 9/27/12 - 9/28/12, .
Tsuji T, Kamei R, Pratt RG. Pore pressure in the nankai trough off the kii peninsula, Japan: Insight into evolution of mega-splay fault. 2012. 論文発表場所 18th Formation Evaluation Symposium of Japan 2012, Chiba, 日本.
Tsuji, Takeshi ; Kamei, Rie ; Pratt, R. Gerhard. / Pore pressure in the nankai trough off the kii peninsula, Japan : Insight into evolution of mega-splay fault. 論文発表場所 18th Formation Evaluation Symposium of Japan 2012, Chiba, 日本.
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