Continental Margin Structure

Continental Margin Structure is the three-dimensional tectonic and stratigraphic architecture of the crust and upper mantle across a continental margin, encompassing the configuration of basement, sedimentary sequences, and deformation and magmatic features that accommodate the transition from continental to oceanic lithosphere.

5.3K

Publications

382.6K

Citations

11.1K

Authors

1.9K

Institutions

Publications per year

2017–2026

784

Authors

11.1K

  1. AB
    A. B. Watts

    University of Oxford, United Kingdom

    37 publications · 4.4K citations

    33

    h-index

  2. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    32 publications · 2.5K citations

    26

    h-index

  3. JI
    Jan Inge Faleide

    University of Oslo, Norway

    31 publications · 2.4K citations

    25

    h-index

  4. GM
    Giänreto Manatschal

    Université de Strasbourg, France

    31 publications · 2.3K citations

    24

    h-index

  5. CE
    C. E. Keen

    Bedford Institute of Oceanography, Canada

    28 publications · 2.4K citations

    23

    h-index

1–5 of 11.1K

Venues

  1. Tectonophysics

    493 publications · 35.7K citations

    101

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 177 publications · 21.5K citations

    82

    h-index

  3. Tectonics

    230 publications · 23.2K citations

    79

    h-index

  4. Geological Society London Special Publications

    224 publications · 17.8K citations

    75

    h-index

  5. Geology

    171 publications · 15.4K citations

    73

    h-index

1–5