Canyon-flank Instability
Canyon-Flank Instability is a geological phenomenon characterized by the progressive weakening and failure of submarine slope materials along the margins of underwater canyons, distinguished from other forms of seafloor instability by its confinement to canyon wall environments and its sensitivity to sediment overloading, fluid migration, and topographically induced stress concentration.
13
Publications
782
Citations
39
Authors
38
Institutions
Publications per year
2017–2026
1
Parents
13
Ages of Valles Marineris (Mars) landslides and implications for canyon history
C. Quantin, Pascal Allemand, N. Mangold et al. · Icarus · 2004 · 107 citations
1–5 of 13
39
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Islamic Azad University, Science and Research Branch, Iran
1 publications · 48 citations
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1–5 of 39
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University of Manchester
Manchester, United Kingdom
1 h-index
1 publications
37 citations
Stanford University
Stanford, United States
1 h-index
2 publications
384 citations
Islamic Azad University of Zanjan
Zanjān, Iran
1 h-index
1 publications
48 citations
University of Lisbon
Lisbon, Portugal
1 h-index
2 publications
324 citations
International Institute of Earthquake Engineering and Seismology
Tehran, Iran
1 h-index
1 publications
48 citations
Texas College
Tyler, United States
1 h-index
3 publications
189 citations
HCA Healthcare
Nashville, United States
1 h-index
2 publications
126 citations
Université Claude Bernard Lyon 1
Villeurbanne, France
1 h-index
3 publications
321 citations
1–8 of 38
2 publications · 75 citations
2
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1 publications · 107 citations
1
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1 publications · 11 citations
1
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1 publications · 162 citations
1
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1 publications · 63 citations
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