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• W2056448837 abstract "The Mweelrea Group (Llanvirnian) in the South Mayo Inlier, western Ireland, consists mainly of coarse shallow-water sandstones with minor slates, cobble conglomerates, and ignimbrite tuffs. The Glenummera Formation at the base (up to 600 m), dominantly well-cleaved slates with some slump features, was deposited in a slope to deep marine shelf environment. A coarsening upward sequence at its top reflects the interaction of fluvial and marine processes, coarse clastic sediments having prograded from the southeast. The rest of the Mweelrea Group (2100 m in the northwest) is dominated by coarse trough cross-bedded sandstone with little evidence for channelling. Three lenticular marine slates (Glendavock, Uggool, and Glenconnelly Formations), up to 200 m thick, wedge out to the southeast. A humid alluvial fan-fan-delta model can explain many features of the Mweelrea Group. Fans built out to the northwest into a relatively small basin with negligible tides and moderate wave energy. Marginal sediments were reworked by waves, occasional storms, and a burrowing fauna." @default.
• W2056448837 created "2016-06-24" @default.
• W2056448837 creator A5074481779 @default.
• W2056448837 date "2007-04-30" @default.
• W2056448837 modified "2023-10-14" @default.
• W2056448837 title "Fluvial to marine transition in the Ordovician of Ireland-A humid-region fan-delta?" @default.
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• W2056448837 doi "https://doi.org/10.1002/gj.3350190205" @default.
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