Channel-form Structures
Channel-Form Structures is a sedimentary structure characterized by a three-dimensional, concave-upward geometry formed by the erosional and depositional processes within a confined flow pathway, distinguishing it from other sedimentary structures by its association with fluvial, tidal, or density-driven current systems and its role in indicating paleoflow direction and sediment transport mechanisms.
189
Publications
10.7K
Citations
680
Authors
311
Institutions
Publications per year
2017–2026
35
Variants
Channel-form Sedimentary Structures
Parents
189
Heejin Kim, Abdul Shakoor, Chansun Park et al. · Advanced Functional Materials · 2012 · 395 citations
Natural Sciences, Materials Engineering, Materials Science +17
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680
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311

Chinese Academy of Sciences
Beijing, China
7 h-index
33 publications
2.4K citations

University of Leeds
Leeds, United Kingdom
4 h-index
15 publications
859 citations
Japan Science and Technology Agency
Tokyo, Japan
4 h-index
6 publications
359 citations
University of California, Santa Barbara
Santa Barbara, United States
4 h-index
8 publications
2.3K citations

University of Aberdeen
Aberdeen, United Kingdom
4 h-index
8 publications
440 citations
University of Chinese Academy of Sciences
Beijing, China
4 h-index
17 publications
791 citations
United States Geological Survey
Reston, United States
3 h-index
4 publications
251 citations
University of Wisconsin–Madison
Madison, United States
3 h-index
5 publications
138 citations
1–8 of 311
8 publications · 411 citations
8
h-index
7 publications · 347 citations
7
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6 publications · 280 citations
6
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6 publications · 255 citations
6
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JSR · 5 publications · 321 citations
5
h-index
1–5