Residual Drift
Residual Drift is the permanent lateral deformation of a structure remaining after the cessation of seismic excitation, distinguishing itself from transient drifts by indicating the extent of inelastic damage and potential impairment of post-earthquake usability.
185
Publications
11.1K
Citations
469
Authors
202
Institutions
Publications per year
2017–2026
92
Variants
Permanent DisplacementPermanent Drift
185
1–5 of 185
469
Universidad Michoacana de San Nicolás de Hidalgo, Mexico
8 publications · 528 citations
8
h-index
7
h-index
6
h-index
University of British Columbia, Okanagan Campus, Canada
5 publications · 423 citations
5
h-index
4
h-index
1–5 of 469
202
Tongji University
Shanghai, China
11 h-index
27 publications
1K citations
Stanford University
Stanford, United States
10 h-index
17 publications
1.7K citations

Southeast University
Nanjing, China
8 h-index
18 publications
350 citations
Virginia Tech
Blacksburg, United States
7 h-index
12 publications
677 citations
University of British Columbia, Okanagan Campus
Kelowna, Canada
7 h-index
11 publications
702 citations
University of Nevada, Reno
Reno, United States
7 h-index
9 publications
539 citations
University at Buffalo, State University of New York
Buffalo, United States
7 h-index
13 publications
2.2K citations
Imam Khomeini International University
Qazvin, Iran
6 h-index
14 publications
649 citations
1–8 of 202
29 publications · 2.7K citations
24
h-index
22 publications · 1.6K citations
18
h-index
9 publications · 773 citations
9
h-index
9 publications · 691 citations
9
h-index
6 publications · 299 citations
6
h-index
1–5