Prograde Reaction Pathways

Prograde Reaction Pathways is a metamorphic reaction sequence that occurs during progressive burial and heating of rocks, distinguished from other reaction pathways by its occurrence under increasing temperature and pressure conditions that drive mineralogical transformations toward higher-grade assemblages.

51

Publications

3.4K

Citations

117

Authors

76

Institutions

Publications per year

2017–2026

2

Authors

117

  1. DR
    David R.M. Pattison

    University of Calgary, Canada

    3 publications · 252 citations

    3

    h-index

  2. WD
    William D. Carlson

    The University of Texas at Austin, United States

    2 publications · 118 citations

    2

    h-index

  3. MI
    Maria Iole Spalla

    University of Milan, Italy

    2 publications · 65 citations

    2

    h-index

  4. DR
    Donald R. Peacor

    University of Michigan, United States

    2 publications · 80 citations

    2

    h-index

  5. AT
    Akira Takasu

    Shimane University, Japan

    2 publications · 122 citations

    2

    h-index

1–5 of 117

Venues

  1. Journal of Metamorphic Geology

    14 publications · 1K citations

    13

    h-index

  2. Journal of Petrology

    3 publications · 424 citations

    3

    h-index

  3. Contributions to Mineralogy and Petrology

    3 publications · 591 citations

    3

    h-index

  4. Lithos

    3 publications · 133 citations

    3

    h-index

  5. American Journal of Science

    2 publications · 194 citations

    2

    h-index

1–5