Andean-type Orogeny

Andean-Type Orogeny is a tectonic process characterized by mountain building at convergent plate boundaries where oceanic lithosphere subducts beneath continental lithosphere, resulting in crustal thickening, magmatic arc development, and uplift without significant continent-continent collision.

655

Publications

54.4K

Citations

2.1K

Authors

643

Institutions

Publications per year

2017–2026

127

Variants

Andean-style Orogeny

Authors

2.1K

  1. VA
    Víctor A. Ramos

    Universidad de Buenos Aires, Argentina

    11 publications · 882 citations

    11

    h-index

  2. AF
    Andrés Folguera

    Universidad de Buenos Aires, Argentina

    9 publications · 567 citations

    9

    h-index

  3. RC
    Reynaldo Charrier

    University of Chile, Chile

    7 publications · 598 citations

    7

    h-index

  4. VV
    V. Valencia

    Washington State University, United States

    6 publications · 346 citations

    6

    h-index

  5. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    6 publications · 1.2K citations

    6

    h-index

1–5 of 2.1K

Venues

  1. Tectonophysics

    67 publications · 7K citations

    43

    h-index

  2. Precambrian Research

    55 publications · 4.8K citations

    40

    h-index

  3. Gondwana Research

    42 publications · 4.1K citations

    34

    h-index

  4. Geological Society of America Bulletin

    38 publications · 4.6K citations

    31

    h-index

  5. Geology

    35 publications · 5K citations

    30

    h-index

1–5