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- W2023697148 abstract "Synopsis An area of Dalradian rocks around Loch Creran, Argyll, has been mapped in detail. In this region Bailey (1922) produced a nappe model of two major Dalradian stratigraphic and structural divisions: the Ballappel Foundation and the Iltay Nappe—divided by the Iltay Boundary Slide. Later Voll (1964) interpreted these divisions as stratigraphic equivalents separated by a facies change. The present work shows that the Dalradian rocks are composed of a single stratigraphic column with the ‘Ballappel’ rocks underlying the ‘Iltay’ rocks. The latter can be divided into two successions. The Ardmucknish Succession is the shallow water equivalent of the thicker Creran Succession, deposited on the northwest flank of the subsiding Dalradian trough. There are no nappe divisions, as defined by Bailey and no facies changes, as defined by Voll." @default.
- W2023697148 created "2016-06-24" @default.
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- W2023697148 date "1980-08-01" @default.
- W2023697148 modified "2023-09-27" @default.
- W2023697148 title "The stratigraphy of the Dalradian rocks around Loch Creran, Argyll" @default.
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- W2023697148 doi "https://doi.org/10.1144/sjg16020105" @default.
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