Propylitic Alteration
Propylitic Alteration is a type of hydrothermal alteration characterized by the pervasive replacement of primary minerals in volcanic rocks with chlorite, epidote, calcite, and lesser albite or pyrite, typically occurring in the outer zones of volcanic hydrothermal systems where low-temperature, oxidized, sulfur-poor fluids interact with mafic to intermediate host rocks.
122
Publications
5.9K
Citations
359
Authors
151
Institutions
Publications per year
2017–2026
26
Variants
Propylitization
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359
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151

University of Tasmania
Hobart, Australia
8 h-index
31 publications
3.5K citations

Imperial College London
London, United Kingdom
6 h-index
10 publications
785 citations
Natural History Museum
London, United Kingdom
5 h-index
10 publications
630 citations
Islamic Azad University South Tehran Branch
Tehran, Iran
4 h-index
7 publications
101 citations

Chinese Academy of Sciences
Beijing, China
4 h-index
9 publications
563 citations
Islamic Azad University North Tehran Branch
Tehran, Iran
4 h-index
7 publications
118 citations
Islamic Azad University, Science and Research Branch
Tehran, Iran
4 h-index
8 publications
123 citations

James Cook University
Townsville, Australia
4 h-index
6 publications
207 citations
1–8 of 151
53 publications · 3.9K citations
32
h-index
5 publications · 155 citations
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GEEA · 4 publications · 240 citations
4
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OJG · 4 publications · 76 citations
4
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3 publications · 298 citations
3
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1–5