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Using seismic scale cliff exposures of Namurian strata, the course will demonstrate depositional complexities and syndepositional deformation structures that characterise delta-slope-turbidite successions
Exposures include 200m high cliffs of Carboniferous strata of County Clare currently undergoing intensive research and recently highlighted in an article in the AAPG Explorer magazine. They comprise some of the most spectacular sedimentary geology in Western Europe, displaying a wide range of delta, slope and turbidite facies and sequences enabling reconstruction of the infilling a major northern Europe basin. Cyclicity of the deltaic succession is thought to have been driven eustatic sea-level changes resulting in extensive flooding surfaces overlain by fossiliferous marine bands and in major palaeovalley fill sandbodies. The deltaic intervals show abundant soft-sediment deformation, egs. growth faults, mud diapirs, sand volcanoes. The course will include at least one boat trip to view key cliff exposures.
Course base: Kilkee, County Clare
Petroleum geologists, general geologists, sedimentologists, reservoir modellers, reservoir engineers.
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