@article{oai:niigata-u.repo.nii.ac.jp:00003221,
 author = {片岡, 香子 and 中条, 武司},
 issue = {12},
 journal = {地質学雑誌, 地質学雑誌},
 month = {Dec},
 note = {Hyperconcentrated flow deposit, in the Ebisutoge-Fukuda tephra from Mie Prefecture, is thought to be deposited from dilution of the debris flow. Debris-flow deposit (facies A) is overlain by hyperconcentrated flow deposit (facies B). Typical hyperconcentrated flow deposit (facies B1；horizontal bedding Part) changes upward into diluted hyperconcentrated flow deposit (facies B2； scour and fill structure part). These facies characteristics indicate that the debris flow changed through hyperconcentrated flow into normal streamflow by dilution during flow traveling.},
 pages = {897--900},
 title = {鮮新・更新統東海層群中の恵比須峠ー福田テフラ(嘉例川火山灰)における土石流 : ハイパーコンセントレイティッド流堆積物の堆積過程},
 volume = {106},
 year = {2000}
}