Titlebook: Later Proterozoic Stratigraphy of the Northern Atlantic Regions; J. A. Winchester (Lecturer in Geology) Book 1988 Springer Science+Busines

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The Moine rocks of Shetlandnt fault (Fig. 6.1). On shore, in Shetland, this fault follows the line of an earlier fault (the Great Glen Fault) and the resultant displacement on the two faults is sinistral and of a magnitude that allows no correlation across these two faults within Shetland. The two occurrences of Moine rocks a

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The Krummedal supracrustal sequence in East Greenland part comprises crystalline complexes, made up of a variety of gneissic and granitic rocks together with metasedimentary rock types. Late Proterozoic (Eleonore Bay Group) and Lower Palaeozoic sequences outcrop mainly between latitudes 72–74°N, while a broad zone of post-Caledonian sediments (Devonia

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The Appin Groupm Connemara in western Ireland to the Banff coast of north-east Scotland. Possible correlatives of this group also occur in Shetland. The type area from which it takes its name is in the north-western part of Argyllshire (now the south-western part of the Highland Region and the northern part of Str

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The ‘Sparagmites’ of Norway18.1) have been studied since the early decades of last century. The successions of this age in Scandinavia became known as the ‘sparagmites’, after the term ‘sparagmite’ was introduced by Esmark (1829) for the dominant, feldspathic sandstone type of these sequences. At present the ‘sparagmites’ are

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