Rim Uplift
Rim Uplift is a geological structure formed by the transient displacement and permanent deformation of target materials during the excavation stage of impact cratering, distinguished by the outward and upward ejection of crustal rocks surrounding the transient cavity.
16
Publications
780
Citations
39
Authors
32
Institutions
Publications per year
2017–2026
2
Parents
16
GEOPHYSICAL CHARACTERIZATION OF THE CHICXULUB IMPACT CRATER
S. P. S. Gulick, Gail Christeson, P. J. Barton et al. · Reviews of Geophysics · 2013 · 134 citations
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Lunar and Planetary Institute
Houston, United States
3 h-index
3 publications
259 citations
University of Arizona
Tucson, United States
3 h-index
7 publications
140 citations

Western University
London, Canada
2 h-index
2 publications
147 citations
The University of Texas at Austin
Austin, United States
2 h-index
3 publications
291 citations
Geological Survey of Canada
Ottawa, Canada
2 h-index
3 publications
297 citations

University of Freiburg
Freiburg im Breisgau, Germany
2 h-index
6 publications
111 citations
Institute of Geology, China Earthquake Administration
Beijing, China
1 h-index
2 publications
30 citations
China Earthquake Administration
Beijing, China
1 h-index
2 publications
30 citations
1–8 of 32
2 publications · 153 citations
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JGR · 2 publications · 142 citations
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2 publications · 141 citations
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1 publications · 52 citations
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1 publications · 13 citations
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