Ht Metamorphism

HT Metamorphism is a type of regional metamorphism characterized by high temperature relative to pressure, typically associated with deep crustal conditions and the development of metamorphic facies such as granulite and amphibolite, distinguishing it from low-temperature or high-pressure metamorphic regimes.

57

Publications

3.5K

Citations

223

Authors

125

Institutions

Publications per year

2017–2026

9

Variants

High-temperature Metamorphism

Publications

57

1–5 of 57

Authors

223

  1. MP
    Marc Poujol

    Géosciences Rennes, France

    4 publications · 220 citations

    4

    h-index

  2. JR
    Jean‐Claude Ringenbach

    Total (France), France

    4 publications · 200 citations

    4

    h-index

  3. PM
    Patrick Monié

    Université de Montpellier, France

    3 publications · 154 citations

    3

    h-index

  4. AG
    Axel Gerdes

    Goethe University Frankfurt, Germany

    3 publications · 402 citations

    3

    h-index

  5. AL
    Abdeltif Lahfid

    Bureau de Recherches Géologiques et Minières, France

    3 publications · 182 citations

    3

    h-index

1–5 of 223

Venues

  1. Journal of Metamorphic Geology

    6 publications · 342 citations

    6

    h-index

  2. Journal of the Geological Society

    JGS · 5 publications · 402 citations

    5

    h-index

  3. Tectonics

    4 publications · 267 citations

    4

    h-index

  4. Lithos

    4 publications · 92 citations

    4

    h-index

  5. Geodinamica Acta

    3 publications · 66 citations

    3

    h-index

1–5