Planetary Uplift

Planetary Uplift is a tectonic process denoting the large-scale, endogenically driven elevation of planetary crustal sections resulting from internal forces such as mantle convection, lithospheric thickening, or intrusive magmatism, distinguished from surface-erosional or impact-related elevation changes by its intrinsic geodynamic origin.

16

Publications

562

Citations

82

Authors

45

Institutions

Publications per year

2017–2026

5

Authors

82

  1. HZ
    Hanshuo Zhang

    Jilin University, China

    1 publications · 19 citations

    1

    h-index

  2. GS
    Giuseppe Solaro

    Istituto per il Rilevamento Elettromagnetico dell'Ambiente, Italy

    1 publications · 12 citations

    1

    h-index

  3. DM
    Dedalo Marchetti

    Istituto Nazionale di Geofisica e Vulcanologia, Italy

    1 publications · 19 citations

    1

    h-index

  4. XR
    Xavier Robert

    Institut des Sciences de la Terre, France

    1 publications · 48 citations

    1

    h-index

  5. ND
    Ning Ding

    Institute of Applied Physics and Computational Mathematics, China

    1 publications · 13 citations

    1

    h-index

1–5 of 82

Venues

  1. Geology

    3 publications · 133 citations

    3

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 2 publications · 92 citations

    2

    h-index

  3. Icarus

    2 publications · 34 citations

    2

    h-index

  4. 1

    h-index

  5. Nature Communications

    1 publications · 56 citations

    1

    h-index

1–5