Mineral Authigenesis

Mineral Authigenesis is the in situ formation of new minerals within a sedimentary deposit during diagenesis, distinguished from detrital mineral components by precipitating directly from pore fluids under physicochemical conditions characteristic of sediment burial and compaction.

1.9K

Publications

85.4K

Citations

5.2K

Authors

1.3K

Institutions

Publications per year

2017–2026

305

Authors

5.2K

  1. AE
    Anthony E. Fallick

    Scottish Universities Environmental Research Centre, United Kingdom

    14 publications · 392 citations

    12

    h-index

  2. SM
    S. Morad

    Uppsala University, Sweden

    12 publications · 288 citations

    11

    h-index

  3. HG
    Harald G. Dill

    Federal Institute for Geosciences and Natural Resources, Germany

    11 publications · 354 citations

    11

    h-index

  4. RR
    Ross R. Large

    University of Tasmania, Australia

    10 publications · 1.7K citations

    10

    h-index

  5. DR
    Donald R. Peacor

    University of Michigan, United States

    10 publications · 425 citations

    10

    h-index

1–5 of 5.2K

Venues

  1. Geochimica et Cosmochimica Acta

    83 publications · 6.7K citations

    50

    h-index

  2. Economic Geology

    141 publications · 6.9K citations

    44

    h-index

  3. Journal of Sedimentary Research

    JSR · 106 publications · 4K citations

    38

    h-index

  4. Mineralium Deposita

    86 publications · 3.4K citations

    35

    h-index

  5. Ore Geology Reviews

    99 publications · 3.9K citations

    34

    h-index

1–5