Stream‐driven, high‐density gravelly traction carpets: possible deposits in the Trabeg Conglomerate Formation, SW Ireland and some theoretical considerations of their origin
- 1 August 1989
- journal article
- Published by Wiley in Sedimentology
- Vol. 36 (4), 513-530
- https://doi.org/10.1111/j.1365-3091.1989.tb02083.x
Abstract
No abstract availableKeywords
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