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On the Chronological Order of Deposition of the Highland Schists1

Published online by Cambridge University Press:  01 May 2009

Thorolf Vogt
Affiliation:
Trondhjem

Extract

As is well known, the chronological order of deposition of the sediments of that broad band of schists which extends across Scotland from Banffshire and Aberdeenshire in the north-east to Argyllshire in the south-west is a most difficult problem to determine. The noteworthy development that has been made during recent years, leading to a more intimate understanding of the structure of the Southern Highlands, has made this problem much more vital. The question as to the top and bottom of these beds has been much discussed in recent years, and it can not be denied that views have been widely divergent on this matter. When a foreign geologist desires to call attention (through this paper) to certain conditions of fact, it may be pointed out that he is carrying on similar studies of another section—the Norwegian—of this same mountain chain, where one meets similar problems as in the Scottish Highlands.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1930

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Footnotes

1

E. B. Bailey accepts T. Vogt's reinterpretation of the Ballachulish succession, and discusses the consequences in a later paper in this number of the Geol. Mag.—Editor.

References

page 68 note 2 Bailey, E. B., “Recumbent Folds in the Schists of the Scottish Highlands,” Q.J.G.S., vol. lxvi, pp. 586618, 1910;CrossRefGoogle Scholar Bailey, E. B., Maufe, H. B., and others, “The Geology of Ben Nevis and Glencoe,” Expl. of Sheet 53, Mem. Geol. Surv. Scotland, 1916;Google Scholar Bailey, E. B., “The Structure of the South-West Highlands of Scotland,” Q.J.G.S., vol. lxxviii, pp. 82127, 1922.CrossRefGoogle Scholar

page 70 note 1 Read, H. H., “The Geology of the Country around Banff, Huntly, and Turriff,” Expl. of Sheets 86 and 96, Mem. Geol. Surv. Scotland, 1923;Google Scholar Read, H. H., Q.J.G.S., vol. lxxviii, pp. 129–30, 1922.Google Scholar