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- W1974572613 abstract "Abstract The Old Red Sandstone provides a fitting closure to a Caledonian cycle of earth history. It can also be regarded as Hercynian in relationship, passing into the marine sequence above. In reconstructing evolving palaeogeography from Silurian to Carboniferous times one difficulty is to try to approach contemporaneity. The experiment is made of concentrating upon Old Red Sandstone evidence in Ireland. The record of Lower and Middle Old Red Sandstone is meagre, but Upper Old Red Sandstone is meagre, but Upper Old Red Sandstone rocks are well displayed. Palynology now allows reasonable charting of the northward marine transgression which brought about decay of the Old Red Sandstone continent in Late Devonian to Early Carboniferous times. Future deployment of palynological investigations is of critical importance." @default.
- W1974572613 created "2016-06-24" @default.
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- W1974572613 date "1979-01-01" @default.
- W1974572613 modified "2023-09-25" @default.
- W1974572613 title "Augmentation and decay of the Old Red Sandstone continent: Evidence from Ireland" @default.
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- W1974572613 doi "https://doi.org/10.1016/0031-0182(79)90093-2" @default.
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