Continental Crust Composition
Continental Crust Composition is a geological construct that specifies the relative abundance and distribution of chemical elements and mineral phases comprising the continental segment of Earth's outermost solid layer, distinguished from oceanic crust by its markedly felsic character, greater thickness, and enriched concentrations of silica, aluminum, potassium, and sodium.
2.5K
Publications
285.5K
Citations
6.1K
Authors
1.3K
Institutions
Publications per year
2017–2026
617
Parents
2.5K
W. F. McDonough, Shen‐Su Sun · Chemical Geology · 1995 · 13.7K citations
The geochemical evolution of the continental crust
Stuart Ross Taylor, S. M. McLennan · Reviews of Geophysics · 1995 · 4.5K citations
1–5 of 2.5K
6.1K
University of Maryland, College Park, United States
35 publications · 9.6K citations
30
h-index
23
h-index
22
h-index
21
h-index
21
h-index
1–5 of 6.1K
1.3K

Chinese Academy of Sciences
Beijing, China
63 h-index
472 publications
37.9K citations

Australian National University
Canberra, Australia
53 h-index
150 publications
52.3K citations

Centre National de la Recherche Scientifique
Paris, France
53 h-index
275 publications
24.5K citations
China University of Geosciences
Wuhan, China
48 h-index
328 publications
58K citations
Institute of Geology and Geophysics
Beijing, China
45 h-index
153 publications
15.9K citations

Chinese Academy of Geological Sciences
Beijing, China
43 h-index
204 publications
19.2K citations
United States Geological Survey
Reston, United States
41 h-index
112 publications
10.8K citations
University of Science and Technology of China
Hefei, China
38 h-index
195 publications
18.4K citations
1–8 of 1.3K
127 publications · 18K citations
68
h-index
129 publications · 15.3K citations
64
h-index
94 publications · 14.5K citations
59
h-index
111 publications · 18.2K citations
58
h-index
JGR · 74 publications · 10.7K citations
49
h-index
1–5