Tectonic Knickpoint is a geomorphic discontinuity in a river longitudinal profile, distinguished from climatically or lithologically induced knickpoints by its origin in tectonic processes such as faulting, uplift, or regional deformation that perturb base level and drive localized changes in erosion rate.
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2.6K
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186
Authors
105
Institutions
Publications per year
2017–2026
16
Parents
Publications
50
1–5 of 50
Authors
186
- AC
3
h-index
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1–5 of 186
Institutions
105
China Earthquake Administration
Beijing, China
5 h-index
20 publications
584 citations
Institute of Geology, China Earthquake Administration
Beijing, China
4 h-index
11 publications
402 citations
University of Potsdam
Potsdam, Germany
4 h-index
5 publications
162 citations
Imperial College London
London, United Kingdom
3 h-index
4 publications
389 citations
Cardiff University
Cardiff, United Kingdom
2 h-index
4 publications
134 citations
Chinese Academy of Sciences
Beijing, China
2 h-index
6 publications
128 citations
Stanford University
Stanford, United States
2 h-index
2 publications
66 citations
Lehigh University
Bethlehem, United States
2 h-index
4 publications
308 citations
1–8 of 105
Venues
- Journal of Geophysical Research Earth Surface
5 publications · 503 citations
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- Earth Surface Processes and Landforms
5 publications · 163 citations
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- Journal of Geophysical Research Atmospheres
JGR · 4 publications · 510 citations
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- Tectonics
4 publications · 162 citations
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- Geomorphology
4 publications · 137 citations
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