Sole Marks
Sole Marks is a type of sedimentary structure characterized by grooves, scratches, or impressions preserved on the underside of a sedimentary bed, formed by the erosion or loading of an underlying surface prior to the deposition of the overlying layer.
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2017–2026
5
Variants
Sole Markings
Parents
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Sole Markings of Graded Graywacke Beds
Ph. H. Kuenen · The Journal of Geology · 1957 · 141 citations
Melt-out till in the Edmonton area, Alberta, Canada
Canadian Journal of Earth Sciences · 1982 · 132 citations
Jeff Peakall, Jim Best, Jaco H. Baas et al. · Sedimentology · 2020 · 90 citations · Full text
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McMaster University
Hamilton, Canada
2 h-index
2 publications
139 citations

Bangor University
Bangor, United Kingdom
2 h-index
3 publications
184 citations
Geological Survey of India
Kolkata, India
2 h-index
2 publications
113 citations

University of Leeds
Leeds, United Kingdom
2 h-index
4 publications
317 citations
Brock University
Saint Catharines, Canada
2 h-index
2 publications
130 citations
China University of Petroleum, East China
Qingdao, China
1 h-index
2 publications
36 citations
University of West Alabama
Livingston, United States
1 h-index
1 publications
21 citations

St. John's University
New York, United States
1 h-index
1 publications
88 citations
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JSR · 19 publications · 707 citations
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JG · 5 publications · 281 citations
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5 publications · 402 citations
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3 publications · 193 citations
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NZJG · 3 publications · 123 citations
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