Turbidite Facies
Turbidite Facies is a sedimentary facies characterized by deposits of turbidity current flows, distinguished from other facies by its diagnostic sequence of graded bedding, sole marks, and Bouma divisions resulting from subaqueous density underflow deposition.
316
Publications
17.1K
Citations
793
Authors
331
Institutions
Publications per year
2017–2026
41
Parents
316
1–5 of 316
793
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331

University of Leeds
Leeds, United Kingdom
11 h-index
23 publications
2.1K citations

University of Parma
Parma, Italy
9 h-index
26 publications
1.5K citations

University of Liverpool
Liverpool, United Kingdom
9 h-index
16 publications
1.4K citations
Geological Survey of Canada
Ottawa, Canada
9 h-index
12 publications
1.4K citations
United States Geological Survey
Reston, United States
8 h-index
22 publications
990 citations
Stanford University
Stanford, United States
8 h-index
15 publications
1.1K citations
Petrobras (Brazil)
Rio de Janeiro, Brazil
7 h-index
12 publications
480 citations
Bedford Institute of Oceanography
Dartmouth, Canada
7 h-index
10 publications
1.3K citations
1–8 of 331
36 publications · 3.3K citations
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JSR · 30 publications · 1.9K citations
24
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23 publications · 972 citations
20
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17 publications · 1.3K citations
16
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18 publications · 1.6K citations
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