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- W2912678885 abstract "The Pleistocene Borj Edouane in NW Tunisia unit consists of two principal facies associations: (1) calcrete-palustrine-laminar crust facies and (2) microbialites. The laminar crusts consist of millimeter-thick couples (ranging from 0.7 to 3 mm thick) of light (from 0.4 to 2 mm) and dark (from 0.2 to 1 mm) laminae. The laminar alternation represents the succession of events with biological remains under quite hydrodynamic conditions (dark laminae) and of slight erosion and transport episodes by thin water sheets and/or eolian activity (detrital phases, light laminae). The presence of intervening intraclastic-ooidal layers indicate erosive processes and the action of weak sheet flows. The laminar crusts were developed in marginal palustrine environments." @default.
- W2912678885 created "2019-02-21" @default.
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- W2912678885 date "2019-01-01" @default.
- W2912678885 modified "2023-10-01" @default.
- W2912678885 title "Stromatolitic Origin of Laminar Crusts in Palustrine Environments (Pleistocene of Borj Edouana Unit, Northwestern Tunisia)" @default.
- W2912678885 cites W2029306589 @default.
- W2912678885 doi "https://doi.org/10.1007/978-3-030-01452-0_37" @default.
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