Deep-marine Facies
Deep-Marine Facies is a sedimentary facies characterized by lithological and paleontological attributes formed in marine environments deeper than the continental shelf, typically distinguished by fine-grained deposits, mass gravity flow structures, and limited bioturbation indicative of low-energy, aphotic conditions.
126
Publications
4.9K
Citations
361
Authors
187
Institutions
Publications per year
2017–2026
28
Parents
126
1–5 of 126
361
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3
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1–5 of 361
187
China University of Geosciences
Wuhan, China
4 h-index
14 publications
505 citations

China Geological Survey
Beijing, China
4 h-index
9 publications
279 citations
Equinor (Norway)
Stavanger, Norway
3 h-index
5 publications
84 citations
The University of Texas at Arlington
Arlington, United States
3 h-index
3 publications
116 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
3 publications
119 citations

Universiti Teknologi Petronas
Ipoh, Malaysia
3 h-index
21 publications
531 citations

University of the Basque Country
Leioa, Spain
3 h-index
9 publications
429 citations
Czech Academy of Sciences, Institute of Geology
Prague, Czechia
2 h-index
2 publications
182 citations
1–8 of 187
8 publications · 240 citations
8
h-index
7 publications · 243 citations
7
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7 publications · 301 citations
7
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JSR · 6 publications · 295 citations
6
h-index
4 publications · 121 citations
4
h-index
1–5