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

Authors

51

  1. PE
    Philip England

    University of Oxford, United Kingdom

    2 publications · 163 citations

    2

    h-index

  2. FZ
    F. Zeb Page

    University of Wisconsin–Madison, United States

    2 publications · 64 citations

    2

    h-index

  3. DA
    D.R. Athey

    Mathematical Institute of the Slovak Academy of Sciences, Slovakia

    1 publications · 71 citations

    1

    h-index

  4. YS
    Yôtâro Seki

    Saitama University, Japan

    1 publications · 11 citations

    1

    h-index

  5. JM
    John M. Ferry

    Johns Hopkins University, United States

    1 publications · 143 citations

    1

    h-index

1–5 of 51

Venues

  1. Journal of Metamorphic Geology

    3 publications · 114 citations

    3

    h-index

  2. Tectonophysics

    1 publications · 92 citations

    1

    h-index

  3. Nature Geoscience

    1 publications · 126 citations

    1

    h-index

  4. American Mineralogist

    1 publications · 143 citations

    1

    h-index

  5. Geological Journal

    1 publications · 30 citations

    1

    h-index

1–5