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- W1606212470 abstract "The age, stratigraphical context and depositional history of the Lower Miocene Terra Member of the Pakhna Formation of Cyprus remain problematic. A sedimentary boundary between a pelagic chalk of Late Oligocene age (age-equivalent to the upper Lefkara Formation of Cyprus) and an overlying shallow water larger foraminiferal carbonate of Early Miocene age (Terra Member) has been analysed as representative of a stacked sequence of fining-upwards carbonate cycles in western Cyprus. Discrimination of autochthonous and allochthonous components of the foraminiferal assemblages demonstrates that the pelagic chalks were repeatedly re-worked into the shallow water environment populated by the larger foraminifera. The significance of this finding for the Cenozoic development of Cyprus is reviewed." @default.
- W1606212470 created "2016-06-24" @default.
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- W1606212470 date "2006-12-01" @default.
- W1606212470 modified "2023-09-27" @default.
- W1606212470 title "Illusory stratigraphy decoded by Oligocene-Miocene autochthonous and allochthonous foraminifera in the Terra Member, Pakhna Formation (Cyprus)" @default.
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