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9 results on '"Nakai, Shinichi"'

1. A modular and multi‐functional purification strategy that enables a common framework for manufacturing scale integrated and continuous biomanufacturing

Author

Pybus, Leon P., primary, Heise, Charles, additional, Nagy, Tibor, additional, Heeran, Carmen, additional, Dover, Terri, additional, Raven, John, additional, Kori, Junichi, additional, Burton, Graeme, additional, Sakuyama, Hiroshi, additional, Hastings, Benjamin, additional, Lyons, Michelle, additional, Nakai, Shinichi, additional, and Haigh, Jonathan, additional

Published
2024
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5. Development of joints in the Sandankyo Area, Hiroshima Prefecture, Southwest Japan <Articles>

Author

Hirayama, Yasuyuki, Hayashi, Takaya, Nakai, Shinichi, Tsushima, Atsuo, and Oho, Yukimasa

Abstract

Joints are markedly developed in the acidic welded tuff of the Sandankyo Area, Hiroshima Prefecture, Southwest Japan. Six sets of joint are distinguished in this area, namely N-S set, NESW set, NNE-SSW set, NW-SE set, NNW-SSE set, and horizontal set. It is considered that NESW, NNE-SSW, NW-SE, and NNW-SSE sets of joint were formed by the simple shear due to NE-SW strike-slip faulting with right-lateral shear sense. Detailed microscopy shows that N-S and NE-SW sets of joint contain narrow quartz vein with newly recrystallized muscovite, and cut by the other sets. This suggests that, preceding the NE-SW faulting, WNW-ESE extention accompanied with granite porphyry intrusion formed N-S and NE-SW sets of joint.

Published
2009

7. 広島県三段峡地域における節理の形成過程 <論文>

Author

Hirayama, Yasuyuki, Hayashi, Takaya, Nakai, Shinichi, Tsushima, Atsuo, Oho, Yukimasa, Hirayama, Yasuyuki, Hayashi, Takaya, Nakai, Shinichi, Tsushima, Atsuo, and Oho, Yukimasa

Abstract

Joints are markedly developed in the acidic welded tuff of the Sandankyo Area, Hiroshima Prefecture, Southwest Japan. Six sets of joint are distinguished in this area, namely N-S set, NESW set, NNE-SSW set, NW-SE set, NNW-SSE set, and horizontal set. It is considered that NESW, NNE-SSW, NW-SE, and NNW-SSE sets of joint were formed by the simple shear due to NE-SW strike-slip faulting with right-lateral shear sense. Detailed microscopy shows that N-S and NE-SW sets of joint contain narrow quartz vein with newly recrystallized muscovite, and cut by the other sets. This suggests that, preceding the NE-SW faulting, WNW-ESE extention accompanied with granite porphyry intrusion formed N-S and NE-SW sets of joint.

Published
2009

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