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- W2103511323 abstract "Post-Arenig ironstones and associated sediments of North Wales have yielded Upper Llanvirn, Llandeilo and Lower Caradoc acritarch assemblages. The occurrence of most ironstones coincides with a eustatic regression and subsequent transgression, and the emergence to the northwest of the Irish Sea Landmass, the probable source of the iron. The majority of ironstone deposition within the basin was restricted to short-lived local submarine rises most likely produced by synsedimentary faulting." @default.
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- W2103511323 date "1987-04-01" @default.
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- W2103511323 title "Age and controls of ironstone deposition (Ordovician) North Wales" @default.
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- W2103511323 doi "https://doi.org/10.1002/gj.3350220505" @default.
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