Wrinkle Ridges

Wrinkle Ridge is a tectonic landform characterized by low, asymmetric, sinuous topographic highs formed by compressional stresses in volcanic plains, typically on planetary surfaces, distinguishing it from other contractional features through its association with mare basalts and shallow thrust faulting.

134

Publications

7.4K

Citations

326

Authors

173

Institutions

Publications per year

2017–2026

23

Authors

326

  1. TR
    T. R. Watters

    Smithsonian Institution, United States

    12 publications · 862 citations

    11

    h-index

  2. JW
    J. W. Head

    Brown University, United States

    11 publications · 809 citations

    11

    h-index

  3. AT
    A. T. Basilevsky

    V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russia

    7 publications · 271 citations

    7

    h-index

  4. MP
    M. P. Golombek

    Jet Propulsion Laboratory, United States

    7 publications · 972 citations

    7

    h-index

  5. MS
    M. S. Robinson

    Arizona State University, United States

    6 publications · 270 citations

    6

    h-index

1–5 of 326

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 29 publications · 2.9K citations

    26

    h-index

  2. Geophysical Research Letters

    11 publications · 398 citations

    11

    h-index

  3. Icarus

    9 publications · 367 citations

    9

    h-index

  4. Journal of Geophysical Research Planets

    5 publications · 110 citations

    5

    h-index

  5. Geology

    5 publications · 543 citations

    5

    h-index

1–5