Siliciclastic Facies
Siliciclastic Facies is a sedimentary facies characterized by the deposition and accumulation of detrital clastic material derived primarily from the weathering and erosion of pre-existing silicate-rich rocks, distinguished by its mineralogical composition, grain size distribution, and textural maturity within siliciclastic depositional systems.
355
Publications
14.8K
Citations
1.1K
Authors
474
Institutions
Publications per year
2017–2026
59
Parents
355
1–5 of 355
1.1K
Friedrich-Alexander-Universität Erlangen-Nürnberg, Germany
6 publications · 290 citations
6
h-index
5
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5
h-index
Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina
4 publications · 285 citations
4
h-index
4
h-index
1–5 of 1.1K
474
Friedrich-Alexander-Universität Erlangen-Nürnberg
Erlangen, Germany
9 h-index
13 publications
673 citations

Centre National de la Recherche Scientifique
Paris, France
9 h-index
23 publications
637 citations

Chinese Academy of Sciences
Beijing, China
7 h-index
12 publications
324 citations
United States Geological Survey
Reston, United States
7 h-index
16 publications
885 citations
The University of Texas at Austin
Austin, United States
7 h-index
11 publications
530 citations

University of Waikato
Hamilton, New Zealand
7 h-index
19 publications
469 citations
Geological Survey of Canada
Ottawa, Canada
6 h-index
10 publications
425 citations
Equinor (Norway)
Stavanger, Norway
6 h-index
14 publications
878 citations
1–8 of 474
36 publications · 2.3K citations
27
h-index
JSR · 33 publications · 1.1K citations
23
h-index
24 publications · 1.3K citations
19
h-index
16 publications · 785 citations
12
h-index
11 publications · 487 citations
11
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1–5