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Open marine conditions have prevailed in the Atlantic basins since mid-Cretaceous times.
All are characteristic of open marine environments; the zonation is not applicable to strata that accumulated in restricted nearshore or deep-basin facies.
Coast Guard officials soon determined that a transmission about mock hostilities on an open marine channel shortly after 9 30 a.m. had touched off the blaze of worldwide news coverage.
No shell material indicating open marine or reefal origin was identified.
The remaining sequences (DS 4 DS 7) reflect open marine mid to outer ramp settings.
At the late stage of rifting, the weakened activity of faulting made it easy to form open marine shelves.
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From the 1960s, investigators began to recognize that many species of the trilobite order Agnostida have intercontinental distributions in open-marine strata.
b The fault between open-marine shelf deposits and debris flow deposits on slope.
Limestone elements are characterised by an open-marine fauna and represent the preserved expression of maximum transgression.
Late Eocene successions in the Fayum Depression display notable facies transition from open-marine to brackish-marine realms.
Facies associations corresponding to fluvial (A1 A6), estuarine (B1 B5) and open-marine (C1 C4) depositional environments were identified.
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