Peak Rings
Peak Rings is a structural geological feature characterized as a circular or arcuate arrangement of uplifted rock formations within the central region of large impact craters, distinguished from simpler central peaks by its annular morphology resulting from gravitational collapse and dynamic rebound processes during crater formation.
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2.4K
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159
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109
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2017–2026
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The formation of peak rings in large impact craters
Joanna Morgan, S. P. S. Gulick, Timothy J. Bralower et al. · Science · 2016 · 238 citations · Full text
Hollows on Mercury: MESSENGER Evidence for Geologically Recent Volatile-Related Activity
D. T. Blewett, N. L. Chabot, B. W. Denevi et al. · Science · 2011 · 162 citations
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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Imperial College London
London, United Kingdom
15 h-index
34 publications
3.2K citations
Brown University
Providence, United States
11 h-index
22 publications
1.4K citations
The University of Texas at Austin
Austin, United States
10 h-index
20 publications
1.9K citations
Planetary Science Institute
Tucson, United States
7 h-index
12 publications
1K citations

Western University
London, Canada
7 h-index
10 publications
917 citations

University of Freiburg
Freiburg im Breisgau, Germany
6 h-index
12 publications
613 citations
University of Texas Institute for Geophysics
Austin, United States
5 h-index
11 publications
870 citations
Universität Hamburg
Hamburg, Germany
5 h-index
6 publications
591 citations
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JGR · 7 publications · 358 citations
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5 publications · 106 citations
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5 publications · 192 citations
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5 publications · 383 citations
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3 publications · 37 citations
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