Ice-rich Sediments

Ice-Rich Sediments is a geological construct denoting a class of permafrost-affected, unconsolidated materials in which ice constitutes a dominant volumetric phase, typically exceeding 50% by volume, and serves as a defining structural and rheological component distinguishing it from other frozen or ice-poor sediments.

192

Publications

11.7K

Citations

803

Authors

341

Institutions

Publications per year

2017–2026

51

Authors

803

  1. GG
    Guido Grosse

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    14 publications · 963 citations

    14

    h-index

  2. LS
    Lutz Schirrmeister

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    12 publications · 754 citations

    12

    h-index

  3. SW
    Sebastian Wetterich

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    8 publications · 748 citations

    8

    h-index

  4. MU
    Mathias Ulrich

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    6 publications · 537 citations

    6

    h-index

  5. MN
    Mikhail N. Grigoriev

    Melnikov Permafrost Institute of the Siberian Branch of the Russian Academy of Science, Russia

    6 publications · 542 citations

    6

    h-index

1–5 of 803

Venues

  1. Canadian Journal of Earth Sciences

    10 publications · 587 citations

    10

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  2. Permafrost and Periglacial Processes

    9 publications · 608 citations

    9

    h-index

  3. Biogeosciences

    8 publications · 441 citations

    8

    h-index

  4. Frontiers in Earth Science

    7 publications · 362 citations

    7

    h-index

  5. Geological Society London Special Publications

    6 publications · 289 citations

    6

    h-index

1–5