Felsic Magmatism

Felsic Magmatism is a type of magmatic process characterized by the generation, ascent, and emplacement of silica-rich, typically granitic to rhyolitic magmas derived from partial melting of crustal or upper mantle sources under specific thermal and tectonic conditions.

1.3K

Publications

81.5K

Citations

3.7K

Authors

1K

Institutions

Publications per year

2017–2026

283

Authors

3.7K

  1. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    21 publications · 1.1K citations

    17

    h-index

  2. JD
    J. Dostál

    Saint Mary's University, Canada

    10 publications · 311 citations

    10

    h-index

  3. JB
    J. Brendan Murphy

    St. Francis Xavier University, Canada

    10 publications · 354 citations

    10

    h-index

  4. SM
    Sandra M. Barr

    Acadia University, Canada

    10 publications · 308 citations

    10

    h-index

  5. RF
    Roberto F. Weinberg

    Monash University, Australia

    10 publications · 678 citations

    10

    h-index

1–5 of 3.7K

Venues

  1. Journal of Petrology

    63 publications · 6K citations

    39

    h-index

  2. Economic Geology

    73 publications · 5K citations

    36

    h-index

  3. Canadian Journal of Earth Sciences

    79 publications · 2.9K citations

    34

    h-index

  4. Lithos

    52 publications · 2.8K citations

    32

    h-index

  5. Journal of the Geological Society

    JGS · 40 publications · 3.4K citations

    31

    h-index

1–5