Low-grade Alteration
Low-Grade Alteration is a type of hydrothermal alteration process characterized by minimal mineralogical and chemical changes in rocks, typically occurring at low temperatures and pressures, and distinguished from higher-grade alterations by the preservation of original rock textures and the formation of stable clay minerals, chlorite, and epidote without pervasive recrystallization.
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2017–2026
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University of Michigan
Ann Arbor, United States
1 h-index
2 publications
384 citations

Justus-Liebig-Universität Gießen
Giessen, Germany
1 h-index
2 publications
44 citations
Institute of Geology and Mineral Exploration
Acharnes, Greece
1 h-index
1 publications
25 citations

Victoria University
Melbourne, Australia
1 h-index
1 publications
12 citations

University of Otago
Dunedin, New Zealand
1 h-index
1 publications
142 citations
Centre for Research and Technology Hellas
Thessaloniki, Greece
1 h-index
3 publications
75 citations

Washington University in St. Louis
St Louis, United States
1 h-index
1 publications
83 citations

Chinese Academy of Sciences
Beijing, China
1 h-index
1 publications
202 citations
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JGS · 2 publications · 272 citations
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1 publications · 192 citations
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1 publications · 25 citations
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1 publications · 202 citations
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