Sodic Alteration
Sodic Alteration is a type of hydrothermal alteration process in which the host rock undergoes mineralogical and chemical changes predominantly through the introduction of sodium-rich fluids, leading to the formation of sodic minerals such as albite, amphibole, or chlorite, thereby distinguishing it from other alteration types by its characteristic alkali element mobility and mineral assemblage.
63
Publications
3.2K
Citations
179
Authors
87
Institutions
Publications per year
2017–2026
7
Variants
Sodic Metasomatism
Parents
63
1–5 of 63
179
3
h-index
2
h-index
2
h-index
2
h-index
Universidade Estadual de Campinas (UNICAMP), Brazil
2 publications · 133 citations
2
h-index
1–5 of 179
87

James Cook University
Townsville, Australia
6 h-index
22 publications
2.6K citations

Colorado School of Mines
Golden, United States
4 h-index
9 publications
617 citations

University of Tasmania
Hobart, Australia
3 h-index
5 publications
159 citations
China University of Geosciences
Wuhan, China
2 h-index
2 publications
71 citations
Universidade de São Paulo
São Paulo, Brazil
2 h-index
3 publications
168 citations

University of Leicester
Leicester, United Kingdom
2 h-index
3 publications
61 citations
Aristotle University of Thessaloniki
Thessaloniki, Greece
2 h-index
2 publications
102 citations
Iowa State University
Ames, United States
2 h-index
2 publications
102 citations
1–8 of 87
16 publications · 1K citations
14
h-index
5 publications · 194 citations
5
h-index
3 publications · 90 citations
3
h-index
3 publications · 64 citations
3
h-index
3 publications · 234 citations
3
h-index
1–5