Isochemical Metamorphism

Isochemical Metamorphism is a type of metamorphic process in which the bulk chemical composition of a rock remains essentially unchanged during mineralogical and textural transformation under conditions of elevated temperature and pressure, distinguished from allochemical metamorphism by the absence of significant chemical mass transfer.

40

Publications

2.2K

Citations

109

Authors

62

Institutions

Publications per year

2017–2026

2

Authors

109

  1. RC
    Robert C. Newton

    University of Chicago, United States

    2 publications · 592 citations

    2

    h-index

  2. JC
    Jiangfeng Chen

    University of Science and Technology of China, China

    1 publications · 105 citations

    1

    h-index

  3. RS
    R. St J. Lambert

    University of Alberta, Canada

    1 publications · 58 citations

    1

    h-index

  4. PA
    Pura Alfonso

    Universitat Politècnica de Catalunya, Spain

    1 publications · 23 citations

    1

    h-index

  5. CR
    C. R. Evans

    Imperial Oil (Canada), Canada

    1 publications · 58 citations

    1

    h-index

1–5 of 109

Venues

  1. Tectonophysics

    4 publications · 122 citations

    4

    h-index

  2. American Journal of Science

    4 publications · 141 citations

    4

    h-index

  3. Journal of the Geological Society

    JGS · 3 publications · 190 citations

    3

    h-index

  4. Contributions to Mineralogy and Petrology

    3 publications · 200 citations

    3

    h-index

  5. Journal of Petrology

    3 publications · 180 citations

    3

    h-index

1–5