Distributed Afterslip
Distributed Afterslip is a postseismic deformation mechanism characterized by the gradual, aseismic slip occurring over an extended, laterally and vertically distributed region of a fault zone following a major seismic event, distinguished from localized afterslip by its broad spatial distribution and contribution to ongoing crustal strain adjustments.
8
Publications
663
Citations
49
Authors
31
Institutions
Publications per year
2017–2026
4
Parents
8
Bin Zhao, Roland Bürgmann, Dongzhen Wang et al. · Journal of Geophysical Research Solid Earth · 2017 · 117 citations · Full text
1–5 of 8
49
Japan Agency for Marine-Earth Science and Technology, Japan
2 publications · 120 citations
2
h-index
Japan Agency for Marine-Earth Science and Technology, Japan
2 publications · 120 citations
2
h-index
2
h-index
1
h-index
The Abdus Salam International Centre for Theoretical Physics (ICTP), Italy
1 publications · 104 citations
1
h-index
1–5 of 49
31
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
2 h-index
8 publications
480 citations
National Earthquake Response Support Service
Beijing, China
1 h-index
1 publications
117 citations
Government of Nepal
Kathmandu, Nepal
1 h-index
1 publications
104 citations
University of Colorado Boulder
Boulder, United States
1 h-index
2 publications
208 citations

Central Washington University
Ellensburg, United States
1 h-index
1 publications
104 citations

Tokyo Gakugei University
Tokyo, Japan
1 h-index
1 publications
19 citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
1 h-index
2 publications
208 citations
The Abdus Salam International Centre for Theoretical Physics (ICTP)
Trieste, Italy
1 h-index
1 publications
104 citations
1–8 of 31
3 publications · 199 citations
3
h-index
1 publications · 19 citations
1
h-index
1 publications · 117 citations
1
h-index
1 publications · 104 citations
1
h-index
BSSA · 1 publications · 200 citations
1
h-index
1–5