Tectonic Uplift

Tectonic Uplift is the vertically directed geological process resulting in the sustained elevation of Earth's crustal segments due to tectonic forces, distinguished from other forms of surface elevation change by its origin in lithospheric deformation rather than isostatic, erosional, or sedimentary mechanisms.

1.5K

Publications

112.6K

Citations

4.1K

Authors

1.1K

Institutions

Publications per year

2017–2026

223

Authors

4.1K

  1. SC
    Sierd Cloetingh

    Vrije Universiteit Amsterdam, Netherlands

    13 publications · 730 citations

    13

    h-index

  2. RW
    Rob Westaway

    Durham University, United Kingdom

    12 publications · 1.1K citations

    12

    h-index

  3. RG
    Rui Gao

    Chinese Academy of Geological Sciences, China

    10 publications · 367 citations

    10

    h-index

  4. MR
    Manfred R. Strecker

    University of Potsdam, Germany

    9 publications · 1K citations

    9

    h-index

  5. XF
    Xiaomin Fang

    Institute of Tibetan Plateau Research, China

    9 publications · 1.6K citations

    9

    h-index

1–5 of 4.1K

Venues

  1. Tectonics

    99 publications · 12.4K citations

    57

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 80 publications · 8.8K citations

    51

    h-index

  3. Tectonophysics

    78 publications · 4.9K citations

    42

    h-index

  4. Earth and Planetary Science Letters

    53 publications · 6.7K citations

    39

    h-index

  5. Geological Society London Special Publications

    63 publications · 5.1K citations

    39

    h-index

1–5