Subduction-zone Metamorphism

Subduction-Zone Metamorphism is a type of regional metamorphism characterized by high-pressure, low-temperature conditions that occur in convergent plate boundaries where oceanic crust and sediments are subducted to depth, resulting in the formation of diagnostic mineral assemblages such as lawsonite, glaucophane, and jadeite within metamorphic rocks.

817

Publications

54.4K

Citations

2.2K

Authors

660

Institutions

Publications per year

2017–2026

152

Authors

2.2K

  1. YZ
    Yong‐Fei Zheng

    University of Science and Technology of China, China

    16 publications · 2.1K citations

    16

    h-index

  2. TT
    Tatsuki Tsujimori

    Tohoku University, Japan

    13 publications · 1.2K citations

    13

    h-index

  3. JG
    J. G. Liou

    Stanford University, United States

    12 publications · 1.2K citations

    12

    h-index

  4. SM
    Shigenori Maruyama

    Tokyo Institute of Technology, Japan

    9 publications · 1.3K citations

    9

    h-index

  5. GE
    Gray E. Bebout

    Lehigh University, United States

    9 publications · 1.8K citations

    9

    h-index

1–5 of 2.2K

Venues

  1. Journal of Metamorphic Geology

    67 publications · 4K citations

    36

    h-index

  2. Lithos

    52 publications · 3K citations

    30

    h-index

  3. Tectonophysics

    32 publications · 3K citations

    25

    h-index

  4. International Geology Review

    40 publications · 1.7K citations

    23

    h-index

  5. Earth and Planetary Science Letters

    27 publications · 3.2K citations

    22

    h-index

1–5