Horizontal and vertical motion at surface of a gassy ocean sediment layer induced by obliquely incident SV waves-Reference-Cited by-同舟云学术

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Horizontal and vertical motion at surface of a gassy ocean sediment layer induced by obliquely incident SV waves

Published:2017-09 Issue: Volume:227 Page:43-53
ISSN:0013-7952
Container-title:Engineering Geology
language:en
Short-container-title:Engineering Geology

Author:

Chen Weiyun,Huang Yu,Wang Zhihua,He Rui,Chen Guoxing^ORCID,Li Xiaojun

Funder

National Natural Science Foundation of China

Natural Science Foundation of Jiangsu Province

Tongji University

State Key Program of National Natural Science Foundation of China

National Key Basic Research Program of China

Publisher

Elsevier BV

Subject

Geology,Geotechnical Engineering and Engineering Geology

Reference33 articles.

1. Reflection transmission coefficients for a layered fluid sediment overlying a uniform solid substrate;Ainslie;J. Acoust. Soc. Am.,1996

2. Gassy sediment occurrence and properties: northern Gulf of Mexico;Anderson;Geo-Mar. Lett.,1990

3. Bubble populations and acoustic interaction with the gassy floor of Eckernförde Bay;Anderson;Cont. Shelf Res.,1998

4. A model for wave propagation in gassy sediments;Bedford;J. Acoust. Soc. Am.,1983

5. Bulk elastic wave propagation in partially saturated porous solids;Berryman;J. Acoust. Soc. Am.,1988

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