Sedimentary environmental change after the Last Glacial Maximum in the Miyagawa Plain, southwestern coast of the Ise Bay, central Japan-Reference-Cited by-同舟云学术

Sedimentary environmental change after the Last Glacial Maximum in the Miyagawa Plain, southwestern coast of the Ise Bay, central Japan

Published:2021-03-30 Issue:1 Volume:72 Page:65-80
ISSN:1346-4272
Container-title:BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN
language:en
Short-container-title:Bull. Geol. Surv. Japan

Author:

SATO Yoshiki¹,MIZUNO Kiyohide¹,NAKASHIMA Rei¹

Affiliation:

1. AIST, Geological Survey of Japan, Research Institute of Geology and Geoinformation

Publisher

National Institute of Advanced Industrial Science

Subject

General Medicine

Link

https://www.jstage.jst.go.jp/article/bullgsj/72/1/72_65/_pdf

Reference31 articles.

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2. Dalrymple, R.W. (1992) Tidal Depositional Systems. In Walker, R.G. and James, N.P., eds., Facies Models: Response to Sea Level Change. Geological Association of Canada, Newfoundland, 195–218.

3. Davis, R.A. Jr. and Hayes, M.O. (1984) What is a wave-dominated coast?. Marine Geology, 60, 313–329. 10.1016/0025-3227(84)90155-5

4. Progradation of Tateyama Strand Plain System, SW Coast of Boso Peninsula, Central Japan, Triggered by Coseismic Uplifts during the Historical Kanto Earthquakes

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