Facies Equilibrium is a petrological theory that defines the condition under which mineral assemblages in metamorphic rocks achieve thermodynamic equilibrium at specific pressure-temperature conditions characteristic of a particular metamorphic facies.
25
Publications
1.2K
Citations
53
Authors
35
Institutions
Publications per year
2017–2026
3
Variants
Metamorphic Facies Equilibrium
Parents
Publications
25
On the Facies Series in Various Types of Metamorphism
Anna Hietanen · The Journal of Geology · 1967 · 83 citations
1–5 of 25
Authors
53
- RW
3
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- MS
2
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- RP
2
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- JM
2
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- AI
2
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1–5 of 53
Institutions
35
China University of Geosciences (Beijing)
Beijing, China
2 h-index
2 publications
42 citations
Harvard University
Cambridge, United States
2 h-index
3 publications
135 citations
The University of Melbourne
Melbourne, Australia
2 h-index
4 publications
390 citations
University of Cape Town
Rondebosch, South Africa
2 h-index
3 publications
255 citations
Johannes Gutenberg University Mainz
Mainz, Germany
2 h-index
3 publications
144 citations
ETH Zurich
Zurich, Switzerland
1 h-index
1 publications
42 citations
Korea Institute of Geoscience and Mineral Resources
Daejeon, South Korea
1 h-index
1 publications
15 citations
University of Wisconsin–Madison
Madison, United States
1 h-index
1 publications
66 citations
1–8 of 35
Venues
- Journal of Metamorphic Geology
8 publications · 471 citations
8
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- Contributions to Mineralogy and Petrology
5 publications · 217 citations
5
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- The Journal of Geology
JG · 2 publications · 142 citations
2
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- The Canadian Mineralogist
1 publications · 41 citations
1
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- American Journal of Science
1 publications · 74 citations
1
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1–5