Central Uplifts
Central Uplifts is a geological structure characterized by the uplifted central region of a complex impact crater, formed by the rebound of crustal materials following the initial compression and excavation stages of hypervelocity impact events.
79
Publications
3.1K
Citations
236
Authors
113
Institutions
Publications per year
2017–2026
4
Parents
79
Taylor Schildgen, Domenico Cosentino, Bodo Bookhagen et al. · Earth and Planetary Science Letters · 2011 · 226 citations · Full text
D. E. Moser, C. L. Cupelli, I. Barker et al. · Canadian Journal of Earth Sciences · 2011 · 173 citations
Erosion-driven uplift of the modern Central Alps
Jean‐Daniel Champagnac, Fritz Schlunegger, Kevin Norton et al. · Tectonophysics · 2009 · 153 citations
1–5 of 79
236
11
h-index
5
h-index
4
h-index
4
h-index
3
h-index
1–5 of 236
113
Museum für Naturkunde
Berlin, Germany
7 h-index
14 publications
374 citations
Humboldt-Universität zu Berlin
Berlin, Germany
6 h-index
9 publications
240 citations

University of the Witwatersrand
Johannesburg, South Africa
6 h-index
11 publications
424 citations
United States Geological Survey
Reston, United States
5 h-index
11 publications
209 citations
University of New Brunswick
Fredericton, Canada
4 h-index
8 publications
370 citations

Western University
London, Canada
4 h-index
11 publications
1.3K citations

Imperial College London
London, United Kingdom
3 h-index
4 publications
247 citations
China University of Geosciences
Wuhan, China
3 h-index
7 publications
421 citations
1–8 of 113
13 publications · 457 citations
13
h-index
JGR · 5 publications · 181 citations
5
h-index
5 publications · 168 citations
5
h-index
5 publications · 105 citations
5
h-index
5 publications · 382 citations
5
h-index
1–5