Basaltic Volcanism

Basaltic Volcanism is a type of volcanic activity characterized by the eruption of low-viscosity, mafic magma rich in iron and magnesium, originating from partial melting of the upper mantle, which typically forms shield volcanoes and extensive lava flows on planetary surfaces.

2.4K

Publications

149.6K

Citations

6.3K

Authors

1.4K

Institutions

Publications per year

2017–2026

332

Authors

6.3K

  1. IE
    Ian E.M. Smith

    University of Auckland, New Zealand

    24 publications · 1.4K citations

    22

    h-index

  2. BF
    B. F. Houghton

    University of Hawaiʻi at Mānoa, United States

    18 publications · 1.7K citations

    17

    h-index

  3. AA
    Alessandro Aiuppa

    University of Palermo, Italy

    16 publications · 1.5K citations

    15

    h-index

  4. GA
    Greg A. Valentine

    University at Buffalo, State University of New York, United States

    16 publications · 1.3K citations

    15

    h-index

  5. FA
    Frederick A. Frey

    Massachusetts Institute of Technology, United States

    15 publications · 1.3K citations

    15

    h-index

1–5 of 6.3K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 175 publications · 17K citations

    77

    h-index

  2. Journal of Volcanology and Geothermal Research

    190 publications · 11.4K citations

    62

    h-index

  3. Journal of Petrology

    110 publications · 9.9K citations

    58

    h-index

  4. Earth and Planetary Science Letters

    98 publications · 11.6K citations

    57

    h-index

  5. Bulletin of Volcanology

    91 publications · 5.3K citations

    43

    h-index

1–5