Sedimentary Process of a Small Sandy Event Deposit due to a Storm Surge and Storm Waves Generated by a Typhoon:
Author:
Affiliation:
1. Graduate School of Science and Engineering, Ibaraki University
2. Geological Survey of Japan, AIST
Publisher
Tokyo Geographical Society
Subject
Materials Chemistry
Link
https://www.jstage.jst.go.jp/article/jgeography/125/5/125_125.747/_pdf
Reference27 articles.
1. Chan, J.C.L. (2006): Comment on “Changes in tropical cyclone number, duration, and intensity in a warming environment”. Science, 311, 1713b.
2. Davis, R.A.Jr. (1992): Depositional Systems: An Introduction to Sedimentology and Stratigraphy, second ed. Englewood Cliffs: Prentice Hall.
3. Emanuel, K.A. (2005): Increasing destructiveness of tropical cyclones over the past 30 years. Nature, 438, 686-688.
4. FitzGerald, D.M., Fenster, M.S., Argow, B.A. and Buynevich, I.V. (2008): Coastal impacts due to sea-level rise. Annual Review of Earth and Planetary Sciences, 36, 601-647.
5. Folk, R.L. and Ward, W.C. (1957): Brazons River bar: A study in the significance of grain size parameters. Journal of Sedimentary Petrology, 27, 3-26.
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