Crack-filling clays and weathered cracks in the DPRI 1800m core near the Nojima Fault, Japan : Evidence for deep surface-water circulation near an active fault

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概要

• 論文の詳細を見る
• 2001-09-01

著者

• Lin Aiming

  Faculty of Science, Shizuoka University.

• Lin Aiming

  Faculty Of Science Kobe University

• TAKEMURA KEIJI

  Graduate School of Science, Kyoto University

• Takemura Keiji

  Graduate School Of Science Kyoto University

• UDA SHIN-ICHI

  Earthquake Research Institute, University of Tokyo

• Uda Shin-ichi

  Earthquake Research Institute University Of Tokyo

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• Paleoseismic events and the 1956 Keicho-Fushimi large earthquake produced by a slip on the Gosukebashi fault at the eastern Rokko Mountains, Japan
• Deformation mechanisms and fluid behavior in a shallow, brittle fault zone during coseismic and interseismic periods : Results from drill core penetrating the Nojima Fault, Japan
• Comparative study of cataclastic rocks from a drill core and outcrops of the Nojima Fault zone on Awaji Island, Japan
• Quaternary vertical offset and average slip rate of the Nojima Fault on Awaji Island, Japan
• Crack-filling clays and weathered cracks in the DPRI 1800m core near the Nojima Fault, Japan : Evidence for deep surface-water circulation near an active fault

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