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.
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3.4K
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119
Authors
51
Institutions
Publications per year
2017–2026
4
Variants
Parallel Laminae
Parents
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51
Shinshu University
Matsumoto, Japan
2 h-index
2 publications
138 citations
Chulalongkorn University
Bangkok, Thailand
2 h-index
15 publications
1K citations

McMaster University
Hamilton, Canada
2 h-index
3 publications
1.1K citations
Seoul National University
Seoul, South Korea
2 h-index
6 publications
578 citations
University of Reading
Reading, United Kingdom
2 h-index
2 publications
132 citations

Jadavpur University
Kolkata, India
2 h-index
5 publications
126 citations
University of Tsukuba
Tsukuba, Japan
2 h-index
3 publications
198 citations
Henan Polytechnic University
Jiaozuo, China
1 h-index
1 publications
17 citations
1–8 of 51
JSR · 12 publications · 649 citations
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8 publications · 1.1K citations
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3 publications · 707 citations
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2 publications · 56 citations
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2 publications · 106 citations
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