Bottom Marks
Bottom Marks is a sedimentary structure characterized by groove-like impressions formed on the undersurface of a bed that record the interaction of fluid flow with the depositional substrate, distinguishing it from other trace fossils or bedforms by its origin as a negative relief feature preserved on the sole of a sedimentary layer.
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Publications
92
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12
Authors
5
Institutions
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2017–2026
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3
Samaneh Masoumi, Lars Reuning, Stefan Back et al. · International Journal of Earth Sciences · 2013 · 25 citations · Full text
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Council for Scientific and Industrial Research, South Africa
1 publications · 34 citations
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Equinor (Norway)
Stavanger, Norway
1 h-index
1 publications
33 citations
University of Bergen
Bergen, Norway
1 h-index
4 publications
132 citations
Maersk (Denmark)
Copenhagen, Denmark
1 h-index
1 publications
25 citations

Council for Scientific and Industrial Research
Pretoria, South Africa
1 h-index
3 publications
102 citations
RWTH Aachen University
Aachen, Germany
1 h-index
4 publications
100 citations
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GR · 1 publications · 25 citations
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1 publications · 33 citations
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1 publications · 34 citations
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