Duricrust Formation

Duricrust Formation is a geological process constituting a type of residual ore deposit formation characterized by the in situ enrichment and cementation of insoluble minerals, particularly oxides and hydroxides of iron, aluminum, or silica, within the regolith through prolonged weathering under arid to semi-arid climatic conditions.

59

Publications

2.6K

Citations

180

Authors

91

Institutions

Publications per year

2017–2026

8

Authors

180

  1. PV
    Paulo Vasconcelos

    The University of Queensland, Australia

    3 publications · 175 citations

    3

    h-index

  2. DJ
    David J. Nash

    University of Brighton, United Kingdom

    3 publications · 213 citations

    3

    h-index

  3. EJ
    Emma J. Gagen

    The University of Queensland, Australia

    3 publications · 130 citations

    3

    h-index

  4. GS
    Gordon Southam

    The University of Queensland, Australia

    3 publications · 130 citations

    3

    h-index

  5. ER
    Erick Ramanaïdou

    Commonwealth Scientific and Industrial Research Organisation, Australia

    2 publications · 90 citations

    2

    h-index

1–5 of 180

Venues

  1. Australian Journal of Earth Sciences

    4 publications · 140 citations

    4

    h-index

  2. Soil Research

    3 publications · 106 citations

    3

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 3 publications · 567 citations

    3

    h-index

  4. Chemical Geology

    3 publications · 132 citations

    3

    h-index

  5. Geochemistry Exploration Environment Analysis

    GEEA · 3 publications · 98 citations

    3

    h-index

1–5