O-222 Are thrust duplexes and contorted beds in the Kotto Unit of Pleiocene Chikura Group of gravitational or tectonic origin?

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概要

• 論文の詳細を見る
• 日本地質学会の論文
• 2001-09-20

著者

• Ogawa Yujiro

  Doctoral Program In Earth Evolution Sciences Graduate School Of Life And Environmental Sciences Univ

• Than Tin

  Doctoral Program In Geoscience And Institute Of Geoscience University Of Tsukuba

• Ogawa Yujiro

  Doctoral Program In Geoscience And Institute Of Geoscience University Of Tsukuba

関連論文

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• Transpressional tectonics of the Mineoka Ophiolite Belt in a trench-trench-trench-type triple junction, Boso Peninsula, Japan
• Large-scale chaotically mixed sedimentary body within the Late Pliocene to Pleistocene Chikura Group, Central Japan
• Origin of layering in cumulate gabbros in the Oman ophiolite : Insights from magnetic susceptibility measurements in the Wadi Sadm area
• O-222 Are thrust duplexes and contorted beds in the Kotto Unit of Pleiocene Chikura Group of gravitational or tectonic origin?

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