Infrasound/seismic observation of the Hayabusa reentry : Observations and preliminary results
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概要
- 論文の詳細を見る
- 2012-07-01
著者
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ISHIHARA Yoshiaki
RISE Project, National Astronomical Observatory of Japan
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FUJITA Kazuhisa
Aerospace Research and Development Directorate, Japan Aerospace Exploration Agency
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Ishihara Yoshiaki
Rise Project National Astronomical Observatory Of Japan
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Hiramatsu Yoshihiro
School Of Natural System College Of Science And Engineering Kanazawa University
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Furumoto Muneyoshi
Graduate School Of Environmental Sciences Nagoya University
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Fujita Kazuhisa
Aerospace Research And Development Directorate Japan Aerospace Exploration Agency
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FURUMOTO Muneyoshi
Graduate School of Environmental Studies, Nagoya University
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Yamamoto Masa-yuki
School of Systems Engineering, Kochi University of Technology
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Hiramatsu Yoshihiro
School of Natural System, College of Science and Engineering, Kanazawa University
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- Is the Ryukyu subduction zone in Japan coupled or decoupled? : The necessity of seafloor crustal deformation observation
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- Shear-wave splitting analysis of the upper mantle at the Niigata-Kobe Tectonic Zone with the data of the Joint Seismic Observations at NKTZ
- Development of Shock Tube for Ground Testing Reentry Aerothermodynamics
- Near-Ultraviolet and Visible Spectroscopy of HAYABUSA Spacecraft Re-Entry
- An Overview of JAXA's Ground-Observation Activities for HAYABUSA Reentry
- Trajectory of HAYABUSA Reentry Determined from Multisite TV Observations
- Detection of Acoustic/Infrasonic/Seismic Waves Generated by Hypersonic Re-Entry of the HAYABUSA Capsule and Fragmented Parts of the Spacecraft
- Tail-wing Flutter Analyses of a Balloon-based Operation Vehicle for Microgravity Experiments
- Infrasound/seismic observation of the Hayabusa reentry : Observations and preliminary results
- Spatial variation in coda Q and stressing rate around the Atotsugawa fault zone in a high strain rate zone, central Japan
- Tail-wing Flutter Analyses of a Balloon-based Operation Vehicle for Microgravity Experiments
- The 1998 Miyako fireball's trajectory determined from shock wave records of a dense seismic array