Orogenic Sediment Supply

Orogenic Sediment Supply is a geological process denoting the flux of detrital material derived from the erosion of mountain belts formed by tectonic convergence, distinguished by its direct linkage to uplift-driven denudation and terrigenous input into adjacent sedimentary basins.

98

Publications

6.3K

Citations

363

Authors

178

Institutions

Publications per year

2017–2026

20

Authors

363

  1. EG
    Eduardo Garzanti

    University of Milano-Bicocca, Italy

    5 publications · 323 citations

    5

    h-index

  2. AR
    Alberto Resentini

    University of Milano-Bicocca, Italy

    4 publications · 158 citations

    4

    h-index

  3. GV
    Giovanni Vezzoli

    University of Milano-Bicocca, Italy

    4 publications · 310 citations

    4

    h-index

  4. JA
    James A. Spotila

    Virginia Tech, United States

    2 publications · 62 citations

    2

    h-index

  5. SS
    Shu Sun

    Institute of Geology and Geophysics, China

    2 publications · 36 citations

    2

    h-index

1–5 of 363

Venues

  1. Sedimentary Geology

    7 publications · 409 citations

    7

    h-index

  2. Journal of Asian Earth Sciences

    6 publications · 150 citations

    6

    h-index

  3. Basin Research

    4 publications · 288 citations

    4

    h-index

  4. Geological Society London Special Publications

    4 publications · 332 citations

    4

    h-index

  5. International Journal of Earth Sciences

    GR · 4 publications · 158 citations

    4

    h-index

1–5