Hematite Remanence

Hematite Remanence is a type of remanent magnetization characterized by the stable magnetic remanence carried by hematite (α-Fe₂O₃) minerals due to their permanent magnetic moments acquired under ambient geological conditions, distinguishing it from other remanence types by its strong anisotropy and high coercivity linked to the mineral’s rhombohedral crystal structure.

85

Publications

3.1K

Citations

184

Authors

109

Institutions

Publications per year

2017–2026

6

Authors

184

  1. SA
    S. A. McEnroe

    Geological Survey of Norway, Norway

    8 publications · 500 citations

    8

    h-index

  2. DJ
    David J. Dunlop

    University of Toronto, Canada

    5 publications · 318 citations

    5

    h-index

  3. PR
    Peter Robinson

    Geological Survey of Norway, Norway

    5 publications · 385 citations

    5

    h-index

  4. MJ
    Mark J. Dekkers

    Utrecht University, Netherlands

    4 publications · 223 citations

    4

    h-index

  5. DT
    D. T. A. Symons

    University of Windsor, Canada

    4 publications · 112 citations

    4

    h-index

1–5 of 184

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 16 publications · 634 citations

    14

    h-index

  2. Geophysical Research Letters

    9 publications · 326 citations

    9

    h-index

  3. Canadian Journal of Earth Sciences

    9 publications · 211 citations

    9

    h-index

  4. Geophysical Journal International

    GJI · 8 publications · 175 citations

    8

    h-index

  5. Earth and Planetary Science Letters

    5 publications · 248 citations

    5

    h-index

1–5