Beach lamination: Nature and origin

H.E. Clifton

doi:10.1016/0025-3227(69)90023-1

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Beach lamination: Nature and origin

Marine Geology

By: H.E. Clifton

https://doi.org/10.1016/0025-3227(69)90023-1

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Abstract

A distinctive two-fold sedimentation unit characterizes lamination in the upper swash zone of beaches. Within the unit a fine and/or a heavy mineral rich layer at the base grades upward into a coarser and/or a heavy mineral poor layer at the top. This distinctive type of lamination results from grain segregation within bed flow during wave backwash.

Additional publication details
Publication type	Article
Publication Subtype	Journal Article
Title	Beach lamination: Nature and origin
Series title	Marine Geology
DOI	10.1016/0025-3227(69)90023-1
Volume	7
Issue	6
Year Published	1969
Language	English
Publisher	Elsevier
Description	7 p.
First page	553
Last page	559