Retrograde Alteration

Retrograde Alteration is a hydrothermal alteration process occurring during the waning stages of skarn formation, characterized by the replacement of high-temperature, anhydrous minerals with lower-temperature, hydrous mineral assemblages due to decreasing temperature and the influx of externally derived, typically more aqueous and cooler fluids.

102

Publications

5K

Citations

347

Authors

191

Institutions

Publications per year

2017–2026

10

Variants

Retrograde Metasomatism

Authors

347

  1. FN
    Fernando Nieto

    Universidad de Granada, Spain

    3 publications · 147 citations

    3

    h-index

  2. DR
    Donald R. Peacor

    University of Michigan, United States

    2 publications · 135 citations

    2

    h-index

  3. PS
    Pulak Sengupta

    Jadavpur University, India

    2 publications · 192 citations

    2

    h-index

  4. LD
    Lawrence D. Meinert

    Washington State University, United States

    2 publications · 320 citations

    2

    h-index

  5. TK
    T. Kurtis Kyser

    Queen's University, Canada

    2 publications · 53 citations

    2

    h-index

1–5 of 347

Venues

  1. Journal of Metamorphic Geology

    13 publications · 714 citations

    12

    h-index

  2. The Journal of Comparative Neurology

    6 publications · 303 citations

    6

    h-index

  3. Mineralogical Magazine

    5 publications · 123 citations

    5

    h-index

  4. Economic Geology

    5 publications · 405 citations

    5

    h-index

  5. Journal of Petrology

    4 publications · 278 citations

    4

    h-index

1–5