Transition Zone Structure

Transition Zone Structure is a seismological construct that characterizes the compositional, thermal, and mineralogical layering within the Earth's mantle between approximately 410 and 660 kilometers depth, distinguished by seismic velocity discontinuities primarily caused by phase transitions in olivine and other mantle silicates.

706

Publications

48.6K

Citations

2.2K

Authors

774

Institutions

Publications per year

2017–2026

139

Authors

2.2K

  1. AN
    A. Nyblade

    Pennsylvania State University, United States

    10 publications · 669 citations

    10

    h-index

  2. KH
    Kelly H. Liu

    Missouri University of Science and Technology, United States

    9 publications · 561 citations

    9

    h-index

  3. SS
    Stephen S. Gao

    Missouri University of Science and Technology, United States

    9 publications · 561 citations

    9

    h-index

  4. AD
    Arwen Deuss

    University of Cambridge, United Kingdom

    8 publications · 706 citations

    8

    h-index

  5. PM
    Peter M. Shearer

    Scripps Institution of Oceanography, United States

    8 publications · 1.3K citations

    8

    h-index

1–5 of 2.2K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 62 publications · 8.2K citations

    45

    h-index

  2. Earth and Planetary Science Letters

    55 publications · 3.5K citations

    37

    h-index

  3. Geophysical Research Letters

    49 publications · 2.5K citations

    30

    h-index

  4. Geophysical Journal International

    GJI · 46 publications · 2.1K citations

    26

    h-index

  5. Physics of The Earth and Planetary Interiors

    20 publications · 1.6K citations

    17

    h-index

1–5