Fault Zone Attenuation is a geophysical phenomenon characterized by the reduction in seismic wave amplitude and energy as waves propagate through a fault zone, distinguished from other forms of seismic attenuation by its dependence on the fault zone's intrinsic structural complexity, fracture density, and fluid content.
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2017–2026
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Institutions
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Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
4 h-index
8 publications
340 citations
United States Geological Survey
Reston, United States
4 h-index
8 publications
314 citations
Istanbul Technical University
Istanbul, Türkiye
3 h-index
7 publications
160 citations
China Earthquake Administration
Beijing, China
3 h-index
11 publications
324 citations
University of Salerno
Fisciano, Italy
3 h-index
4 publications
88 citations
University of Aberdeen
Aberdeen, United Kingdom
2 h-index
5 publications
165 citations
Institute of the Earth’s Crust
Irkutsk, Russia
2 h-index
2 publications
55 citations
Universidad Nacional Autónoma de México
Mexico City, Mexico
2 h-index
4 publications
258 citations
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Venues
- Bulletin of the Seismological Society of America
BSSA · 9 publications · 577 citations
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- Tectonophysics
4 publications · 167 citations
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- Journal of Geophysical Research Atmospheres
JGR · 4 publications · 483 citations
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- Physics of The Earth and Planetary Interiors
3 publications · 204 citations
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- Geophysical Journal International
GJI · 3 publications · 125 citations
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