High-pressure Metamorphism

High-Pressure Metamorphism is a type of metamorphic process characterized by mineralogical and chemical transformations occurring under unusually elevated pressure conditions, typically associated with subduction zones or continental collision settings, where the dominant variable distinguishing it from other metamorphic pathways is the exceptionally high pressure relative to temperature.

784

Publications

55.2K

Citations

1.8K

Authors

593

Institutions

Publications per year

2017–2026

99

Authors

1.8K

  1. JG
    J. G. Liou

    Stanford University, United States

    13 publications · 1.8K citations

    13

    h-index

  2. BG
    Bruno Goffé

    Laboratoire de Géologie de l’École Normale Supérieure, France

    11 publications · 1.2K citations

    11

    h-index

  3. HM
    Hans‐Joachim Massonne

    University of Stuttgart, Germany

    12 publications · 516 citations

    11

    h-index

  4. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    10 publications · 640 citations

    10

    h-index

  5. JA
    Jane A. Gilotti

    University of Iowa, United States

    8 publications · 536 citations

    8

    h-index

1–5 of 1.8K

Venues

  1. Contributions to Mineralogy and Petrology

    46 publications · 4.5K citations

    36

    h-index

  2. Geology

    34 publications · 3.1K citations

    30

    h-index

  3. Journal of Petrology

    34 publications · 4.2K citations

    27

    h-index

  4. Lithos

    42 publications · 2.9K citations

    27

    h-index

  5. Journal of Metamorphic Geology

    37 publications · 1.9K citations

    26

    h-index

1–5