Breakup Processes

Breakup Processes is a geophysical phenomenon characterized by the disintegration of continuous lithospheric plates or sea ice covers due to mechanical forcing, thermal gradients, or fluid-induced weakening, distinguished by the progressive fragmentation of cohesive structural units into discrete segments within rift tectonics or sea ice dynamics.

324

Publications

21.5K

Citations

1.1K

Authors

494

Institutions

Publications per year

2017–2026

80

Authors

1.1K

  1. MY
    Masanobu Yahiro

    Kyushu University, Japan

    7 publications · 553 citations

    7

    h-index

  2. MK
    M. Kamimura

    Kyushu University, Japan

    7 publications · 562 citations

    7

    h-index

  3. PR
    P. R. S. Gomes

    Universidade Federal Fluminense, Brazil

    6 publications · 463 citations

    6

    h-index

  4. WG
    W. Glöckle

    Ruhr University Bochum, Germany

    6 publications · 195 citations

    6

    h-index

  5. JL
    J. Lubián

    Universidade Federal Fluminense, Brazil

    5 publications · 355 citations

    5

    h-index

1–5 of 1.1K

Venues

  1. Physical Review C

    PRC · 28 publications · 1.5K citations

    18

    h-index

  2. Physics of Fluids

    14 publications · 796 citations

    13

    h-index

  3. Journal of Fluid Mechanics

    12 publications · 930 citations

    12

    h-index

  4. Atomization and Sprays

    12 publications · 857 citations

    11

    h-index

  5. Physics Letters B

    9 publications · 452 citations

    9

    h-index

1–5