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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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In the Eocene White Limestone Group at Lloyds, southeastern Jamaica, submarine sliding has brought layers of coarse clastic carbonate and non-carbonate material into a sequence of planktonic foraminiferal micrite. It is concluded that there were no nearby land areas at the time the sediments were deposited and that the exotic material was derived from penecontemporaneously formed shallow-water carbonates and from older non-carbonate rocks cropping out on a submarine bank or the edge of a submarine fault scarp.
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