Kentaro Emoto 研究室

AI 要約（直近 5 年の研究成果）

※ AI（Claude）が、公開されている論文要旨から研究の問い・手法・主要な発見を事実情報として抽出・再構成して自動生成しています。誤りを含む可能性があるため、正確性は研究室公式情報でご確認ください。

研究成果（20 件）

• [2026] Coseismic velocity decreases and logarithmic recovery at Sakurajima volcano imaged by DAS-based seismic interferometry
  DOI: https://doi.org/10.5194/egusphere-gc14-fibreoptic-5
• [2026] Tracking volcanic stress and strength changes using the seismic moment ratio (Mstk/M0) at Kirishima volcano, Kyushu, Japan
  DOI: https://doi.org/10.5194/egusphere-egu26-3835
• [2026] Monitoring of volcanic earthquakes and tremor using DAS at Sakurajima volcano, Japan
  DOI: https://doi.org/10.5194/egusphere-gc14-fibreoptic-60
• [2025] Systematic Differences in Energy Radiation Processes Between Regular and Intraplate Low‐Frequency Earthquakes Around the Focal Area of the 2008 Mw ${\boldsymbol{M}}_{\boldsymbol{w}}$ 6.9 Iwate‐Miyagi, Japan, Earthquake
  DOI: https://doi.org/10.1029/2024jb030750
• [2025] Shaking-induced small seismic velocity changes as revealed from seismic interferometry analysis of distributed acoustic sensing data
  DOI: https://doi.org/10.22541/essoar.176521470.09976552/v1
• [2025] Complex principal component analysis of volcanic earthquakes at Azuma volcano, Japan, recorded by a distributed acoustic sensing system (DAS) for the hypocenter determination
  DOI: https://doi.org/10.1016/j.jvolgeores.2025.108343
• [2025] Along‐Dip Variations in Source Characteristics of Shallow Slow Earthquakes Controlled by Topography of Subducted Oceanic Plate
  DOI: https://doi.org/10.1029/2024jb030751
• [2024] Near‐Source Waveform Modeling to Estimate Shallow Crustal Attenuation and Radiated Energy of <i>M</i> _w 2.0–4.5 Earthquakes
  DOI: https://doi.org/10.1029/2023jb028523
• [2024] Estimation of shallow structure along the hinagu fault by applying seismic interferometry to DAS observations conducted along national route 3 in Kumamoto prefecture, Japan
  DOI: https://doi.org/10.1186/s40623-024-02088-3
• [2024] Revisiting Seismic Energy of Shallow Tremors: Amplifications Due To Site and Propagation Path Effects Near the Nankai Trough
  DOI: https://doi.org/10.1029/2024jb029168

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