Fault Fling Step
Fault Fling Step is a geophysical phenomenon in seismology characterized by the sudden static displacement of the ground surface adjacent to a rupturing fault due to tectonic slip, distinguished from dynamic shaking by its permanent, step-like deformation recorded in strong ground motion data.
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1.6K
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2017–2026
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Fling StepNear-fault Fling
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Kogakuin University
Tokyo, Japan
2 h-index
2 publications
131 citations
National Technical University of Athens
Athens, Greece
2 h-index
7 publications
496 citations

The University of Queensland
Brisbane, Australia
1 h-index
2 publications
86 citations
United States Geological Survey
Reston, United States
1 h-index
1 publications
112 citations

American University of Armenia
Yerevan, Armenia
1 h-index
1 publications
139 citations

University of Cagliari
Cagliari, Italy
1 h-index
1 publications
30 citations

Iran University of Science and Technology
Tehran, Iran
1 h-index
3 publications
51 citations
TEPCO (Japan)
Tokyo, Japan
1 h-index
1 publications
24 citations
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BSSA · 4 publications · 257 citations
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5 publications · 284 citations
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2 publications · 637 citations
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2 publications · 153 citations
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1 publications · 15 citations
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