Parallel Lamination

Parallel Lamination is a type of sedimentary structure characterized by thin, parallel layers of fine-grained sediment deposited under steady, unidirectional flow conditions, distinguished from other laminations by the absence of cross-cutting or undulatory patterns.

42

Publications

3.4K

Citations

119

Authors

51

Institutions

Publications per year

2017–2026

4

Variants

Parallel Laminae

Authors

119

  1. RG
    Roger G. Walker

    McMaster University, Canada

    3 publications · 592 citations

    3

    h-index

  2. KJ
    Kruawun Jankaew

    Chulalongkorn University, Thailand

    2 publications · 138 citations

    2

    h-index

  3. RW
    R. W. C. Arnott

    University of Ottawa, Canada

    2 publications · 339 citations

    2

    h-index

  4. SS
    Seung Soo Chun

    Chonnam National University, South Korea

    2 publications · 289 citations

    2

    h-index

  5. MC
    Montri Choowong

    Chulalongkorn University, Thailand

    2 publications · 138 citations

    2

    h-index

1–5 of 119

Venues

  1. Journal of Sedimentary Research

    JSR · 12 publications · 649 citations

    12

    h-index

  2. Sedimentology

    8 publications · 1.1K citations

    8

    h-index

  3. AAPG Bulletin

    3 publications · 707 citations

    3

    h-index

  4. Geological Journal

    2 publications · 56 citations

    2

    h-index

  5. Sedimentary Geology

    2 publications · 106 citations

    2

    h-index

1–5