Near-surface Attenuation
Near-Surface Attenuation is a seismic attenuation phenomenon characterized by the reduction in amplitude and alteration of frequency content of seismic waves as they propagate through the uppermost layers of the Earth's crust, distinguished from deeper attenuation processes by its strong dependence on shallow subsurface heterogeneities, unconsolidated materials, and near-surface geological conditions.
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3.2K
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254
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129
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2017–2026
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Istituto Nazionale di Geofisica e Vulcanologia, Italy
3 publications · 133 citations
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The University of Tokyo
Tokyo, Japan
7 h-index
12 publications
345 citations
Planetary Science Institute
Tucson, United States
5 h-index
5 publications
179 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
7 publications
387 citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
4 h-index
8 publications
369 citations

China University of Petroleum, Beijing
Beijing, China
3 h-index
6 publications
81 citations

Universidad de Granada
Granada, Spain
3 h-index
5 publications
147 citations
University of California, Berkeley
Berkeley, United States
3 h-index
6 publications
152 citations

University of Naples Federico II
Naples, Italy
3 h-index
3 publications
122 citations
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BSSA · 14 publications · 733 citations
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9 publications · 244 citations
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GJI · 6 publications · 199 citations
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5 publications · 208 citations
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5 publications · 250 citations
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