Fault-controlled Relief

Fault-Controlled Relief is a type of tectonic landform characterized by differential elevation across a fault zone, wherein the relief is generated and maintained by displacement along bedrock faults that directly influence the topographic expression of mountainous regions.

10

Publications

325

Citations

29

Authors

17

Institutions

Publications per year

2017–2026

2

Authors

29

  1. PI
    Pablo Iturrieta

    GFZ Helmholtz Centre for Geosciences, Germany

    1 publications · 40 citations

    1

    h-index

  2. JL
    Jean-Marc Lardeaux

    Université Côte d'Azur, France

    1 publications · 11 citations

    1

    h-index

  3. GS
    Gwo-Shyh Song

    National Taiwan University, Taiwan

    1 publications · 15 citations

    1

    h-index

  4. GG
    Gérard Giannérini

    Université Côte d'Azur, France

    1 publications · 11 citations

    1

    h-index

  5. GA
    Gloria Arancibia

    Pontificia Universidad Católica de Chile, Chile

    1 publications · 40 citations

    1

    h-index

1–5 of 29

Venues

  1. Precambrian Research

    1 publications · 13 citations

    1

    h-index

  2. Geosphere

    1 publications · 24 citations

    1

    h-index

  3. Geothermics

    1 publications · 40 citations

    1

    h-index

  4. 1

    h-index

  5. Geophysical Research Letters

    1 publications · 21 citations

    1

    h-index

1–5