High-temperature Element Mobility

High-Temperature Element Mobility is a geochemical process that describes the relative ease and mechanisms by which chemical elements migrate and redistribute in silicate melts, magmatic fluids, and high-grade metamorphic systems under elevated temperature and pressure conditions typical of Earth’s crust and mantle, distinguished from low-temperature mobility processes by the dominant role of thermal energy, ionic diffusion, and phase equilibria in facilitating elemental transport.

11

Publications

749

Citations

44

Authors

24

Institutions

Publications per year

2017–2026

0

Authors

44

  1. CE
    C. E. Manning

    University of California, Los Angeles, United States

    2 publications · 262 citations

    2

    h-index

  2. MJ
    Michael J. Toplis

    Centre National de la Recherche Scientifique, France

    1 publications · 21 citations

    1

    h-index

  3. CS
    Carl Spandler

    James Cook University, Australia

    1 publications · 216 citations

    1

    h-index

  4. AA
    A. Antignano

    University of California, Los Angeles, United States

    1 publications · 190 citations

    1

    h-index

  5. JH
    Jörg Hermann

    Australian National University, Australia

    1 publications · 216 citations

    1

    h-index

1–5 of 44

Venues

  1. Chemical Geology

    4 publications · 512 citations

    4

    h-index

  2. Geochimica et Cosmochimica Acta

    2 publications · 48 citations

    2

    h-index

  3. Journal of Applied Physics

    1 publications · 23 citations

    1

    h-index

  4. The Journal of Physical Chemistry B

    1 publications · 74 citations

    1

    h-index

  5. Lithos

    1 publications · 34 citations

    1

    h-index

1–5