Equilibrium Metamorphism
Equilibrium Metamorphism is a physical process in snowpack stratigraphy whereby snow microstructure evolves toward thermodynamic equilibrium under isothermal or near-isothermal conditions, driven primarily by vapor diffusion to minimize surface energy.
18
Publications
1.5K
Citations
51
Authors
27
Institutions
Publications per year
2017–2026
1
Variants
Equitemperature Metamorphism
Parents
18
An overview of seasonal snow metamorphism
S. C. Colbeck · Reviews of Geophysics · 1982 · 526 citations
Patterns of mineral occurrence in metamorphic rocks
John M. Ferry · American Mineralogist · 2000 · 143 citations
Fluid-driven metamorphism of the continental crust governed by nanoscale fluid flow
Oliver Plümper, Alexandru Boţan, Catharina Los et al. · Nature Geoscience · 2017 · 126 citations · Full text
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Mathematical Institute of the Slovak Academy of Sciences, Slovakia
1 publications · 71 citations
1
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1
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1–5 of 51
27

University of Oslo
Oslo, Norway
1 h-index
3 publications
378 citations
Geophysical Laboratory
Washington, United States
1 h-index
1 publications
20 citations

Kōchi University
Kochi, Japan
1 h-index
1 publications
30 citations

Akebono (Japan)
Hanyū, Japan
1 h-index
1 publications
30 citations

Carnegie Institution for Science
Washington, United States
1 h-index
1 publications
20 citations
Mathematical Institute of the Slovak Academy of Sciences
Bratislava, Slovakia
1 h-index
1 publications
71 citations
Utrecht University
Utrecht, The Netherlands
1 h-index
2 publications
252 citations

University of Montana
Missoula, United States
1 h-index
1 publications
51 citations
1–8 of 27
3 publications · 114 citations
3
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1 publications · 92 citations
1
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1 publications · 126 citations
1
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1 publications · 143 citations
1
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1 publications · 30 citations
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