Uplifting Age of the Hida Range by Investigation of River Terraces and Volcano Geology

  • 藤井, 昭二 (Principal Investigator)

Project Details

Abstract

3) River terraces of Matsumoto basin is differ from one of Toyama Basin. But higher, middle and lower terraces are classified by loam succession. Terraces located only south and west parts of the Matsumoto basin. Higher terraces are few perhaps they eroded out by lifting of Hida range.
StatusFinished
Effective start/end date1988/01/01 → 1990/12/31

Funding

  • Japan Society for the Promotion of Science: ¥1,300,000.00

Keywords

  • 飛騨山脈の隆起
  • 乗鞍火山帯噴出期
  • 立山火山の噴出期
  • 北陸の扇状地
  • 隆起扇状地の数
  • 松本盆地の扇状地
  • 隆起扇状地の段数
  • 松本盆地
  • 河岸段丘
  • アカンダナ火山
  • 安房トンネル
  • 低速度帯
  • 飛騨山脈の隆起と火山活動
  • "立山火山"のK-Ar年代
  • 安房トンネルから発見された木材のC14年代
  • アカンダナ火山の活動
  • Uplifting age
  • Hida range
  • Tateyama volcanos
  • Raised alluvial fan
  • Hokuriku region
  • Matsumoto basin
  • Omine plane
  • River terraces of Matsumoto basin

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