Ground Motion Amplification
Ground Motion Amplification is a geotechnical seismic response phenomenon in which the amplitude of seismic waves increases as they propagate through unconsolidated soil layers overlying bedrock, distinguished by the contrast in impedance between subsurface materials and the resulting resonance effects that intensify surface ground shaking.
430
Publications
24K
Citations
1.1K
Authors
392
Institutions
Publications per year
2017–2026
134
Parents
430
1–5 of 430
1.1K
10
h-index
University of California, Los Angeles, United States
8 publications · 803 citations
8
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8
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7
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Institut de Radioprotection et de Sûreté Nucléaire, France
7 publications · 384 citations
7
h-index
1–5 of 1.1K
392
United States Geological Survey
Reston, United States
24 h-index
86 publications
5.7K citations
University of Southern California
Los Angeles, United States
20 h-index
38 publications
2.7K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
10 h-index
30 publications
2.1K citations

Kyoto University
Kyoto, Japan
10 h-index
26 publications
1.7K citations
Tokyo Institute of Technology
Tokyo, Japan
9 h-index
15 publications
2.1K citations
Institute of Earth Sciences, Academia Sinica
Taipei, Taiwan
9 h-index
18 publications
691 citations
Université Gustave Eiffel
Champs-sur-Marne, France
9 h-index
13 publications
657 citations
University of California, Los Angeles
Los Angeles, United States
8 h-index
12 publications
955 citations
1–8 of 392
BSSA · 107 publications · 10.4K citations
52
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40 publications · 2.1K citations
27
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32 publications · 1.5K citations
22
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26 publications · 1.9K citations
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GJI · 14 publications · 522 citations
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