Rift Margin Architecture

Rift Margin Architecture is a geological framework that characterizes the structural and stratigraphic organization of continental margins formed during rifting, distinguished by the spatial arrangement of fault systems, subsiding basins, and uplifted blocks resulting from lithospheric extension.

528

Publications

37.6K

Citations

1.7K

Authors

620

Institutions

Publications per year

2017–2026

119

Authors

1.7K

  1. GM
    Giänreto Manatschal

    Université de Strasbourg, France

    20 publications · 1.6K citations

    18

    h-index

  2. GP
    Gwenn Péron‐Pinvidic

    Geological Survey of Norway, Norway

    10 publications · 680 citations

    10

    h-index

  3. GC
    Giacomo Corti

    Institute of Geosciences and Earth Resources, Italy

    7 publications · 538 citations

    7

    h-index

  4. CJ
    Christopher Jackson

    Imperial College London, United Kingdom

    6 publications · 284 citations

    6

    h-index

  5. BR
    Bruce R. Rosendahl

    Duke University, United States

    6 publications · 505 citations

    6

    h-index

1–5 of 1.7K

Venues

  1. Tectonophysics

    96 publications · 8.7K citations

    44

    h-index

  2. Marine and Petroleum Geology

    43 publications · 3.1K citations

    32

    h-index

  3. Geology

    22 publications · 1.3K citations

    20

    h-index

  4. Earth and Planetary Science Letters

    19 publications · 1.9K citations

    19

    h-index

  5. Tectonics

    20 publications · 1.2K citations

    19

    h-index

1–5