Core sample of bottom sediment at the northern part of Nakanose,Tokyo Bay.
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Date
1960
Métadonnées
Afficher la notice complèteAbstract
The rate of sedimentation of Tokyo Bay is estimated by means of core analysis as 2.4 cm per 10 years. This rate was determined on the basis of the key bed of scoria layer derived from the Hoei eruption of Mt. Fuji. And, chronological changes of sedimentary environment through the core have been found by the analyses of grain size, minerals, pollen, diatom, and foraminifera.Journal
Report of Hydrographic and Oceanographic ResearchesIssue/Article Nr
2Page Range
pp.87-108Resource/Dataset Location
https://www1.kaiho.mlit.go.jp/GIJUTSUKOKUSAI/KENKYU/report/CMRL2(2)/CMRL2(2)-4.pdf