About a mechanism of the formation of sedimentary waves on the shelf of the Sea of Japan

被引:8
作者
Dolgikh, G. I. [1 ,2 ]
Novotryasov, V. V. [1 ,2 ]
Samchenko, A. N. [1 ]
Yaroshchuk, I. O. [1 ,2 ]
机构
[1] Russian Acad Sci, Far East Branch, Ilichev Pacific Oceanol Inst, Vladivostok 690022, Russia
[2] Far East Fed Univ, Vladivostok, Russia
基金
俄罗斯基础研究基金会; 俄罗斯科学基金会;
关键词
NONLINEAR INTERNAL WAVES;
D O I
10.1134/S1028334X15120090
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The existence of sedimentary waves at depths ranging from 50 to 100 m in Peter the Great Bay of the Sea of Japan has been discovered and substantiated as a result of geological and geophysical experiments. The experimental and theoretical studies have made it possible to conclude that the sedimentary waves form in the depth range specified due to processes related to the disintegration of nonlinear gravity waves.
引用
收藏
页码:1278 / 1282
页数:5
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