Hostname: page-component-cd9895bd7-7cvxr Total loading time: 0 Render date: 2024-12-24T01:10:24.469Z Has data issue: false hasContentIssue false
  • English
  • Français

Age-Problems of the Moine Series of Scotland

Published online by Cambridge University Press:  01 May 2009

H. H. Read
H. H. Read
Affiliation:
Professor of Geology, University of Liverpool.
Get access Rights & Permissions [Opens in a new window]

Extract

The Chapters on the Geology of Scotland, by B. N. Peach and John Home, reveals very clearly the complete divergence in the views of these two masters concerning certain fundamental problems of the Moine Series. Peach (1, pp. 199–200) regards the Moine Series as the equivalent of the Torridonian and its metamorphism as entirely post-Cambrian. Home (1, pp. 200–1), on the other hand, believes the Moine Series to consist mainly of sedimentary schists of pre-Torridonian age which formed part of the land-barrier separating the Cambrian sea in the North-West Highlands from that in which the fossiliferous Highland Border Rocks (Cambro-Ordovician) were laid down.

Type
Original Articles
Information
Geological Magazine , Volume 71 , Issue 7 , July 1934 , pp. 302 - 317
Copyright
Copyright © Cambridge University Press 1934

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

BIBLIOGRAPHY

(1)Peach, B. N. and Horne, J., Chapters on the Geology of Scotland, Oxford University Press, 1930.Google Scholar
(2) “The Geological Structure of the North-West Highlands of Scotland”: Mem. Geol. Surv., 1907.Google Scholar
(3) “The Geology of Strath Oykell and Lower Loch Shin” (Explan. Sheet 102): Mem. Geol. Surv., 1926.Google Scholar
(4)Frödin, G., “On the Analogies between the Scottish and Scandinavian Portions of the Caledonian Mountain Range”: Bull. Geol. Inst. Univ. Uppsala, xviii, 1922, 199–238.Google Scholar
(5)Lapworth, C., “On the Stratigraphy and Metamorphism of the Rocks of the Durness-Eriboll District”: Proc. Geol. Assoc., viii, 1885, 438–442.Google Scholar
(6)von Bubnoff, S., Geotogie von Europa, ii, pt. i.Google Scholar
(7) “The Geology of Glenelg, etc.” (Explan. Sheet 71): Mem. Geol. Surv., 1910.Google Scholar
(8)Gregory, J. W., “Moine Pebbles in Torridonian Conglomerates”: Geol. Mag., 1915, 447.CrossRefGoogle Scholar
(9)Tilley, C. E., “A Preliminary Survey of Metamorphic Zones in the Southern Highlands of Scotland”: Quart. Journ. Geol. Soc., lxxxi, 1925, 100–112.CrossRefGoogle Scholar
(10) “The Geology of the Country around Golspie, Sutherlandshire” (Explan. Sheet 103): Mem. Geol. Surv., 1925.Google Scholar
(11) “The Geology of Central Sutherland” (Explan. Sheets 108 and 109): Mem. Geol. Surv., 1931.Google Scholar
(12) “The Geology of Ben Wyvis, Carn Chuinneag, etc.” (Explan. Sheet 93): Mem. Geol. Surv., 1912.Google Scholar
(13)Clouoh, C. T., Crampton, C. B., and Flett, J. S., “The Augen Gneiss and Moine Sediments of Ross-shire”: Geol. Mag., 1910, 337.CrossRefGoogle Scholar
(14) “The Geology of Central Ross-shire” (Explan. Sheet 82): Mem. Geol. Surv., 1913.Google Scholar
(15)Read, H. H., Abstr. Proc. Geol. Soc., London, No. 1276, 1934.Google Scholar
(16)Suess, F. E., “A Suggested Interpretation of the Scottish Caledonide Structure”: Geol. Mag., 1931, 71–81.CrossRefGoogle Scholar
(17)Wright, W. B., “The Two Earth-movements of Colonsay”: Quart. Journ. Geol. Soc., lxiv, 1908, 297.CrossRefGoogle Scholar
(18) Annual Report of the Geological Survey for 1892, 1893, 262.Google Scholar
(19) (Sir) Flett, J. S., “On the Petrographical Characters of the Inliers of Lewisian Rocks among the Moine Gneisses of the North of Scotland”: Summary of Progress for 1905, Mem. Geol. Surv., 1906, 155.Google Scholar
(20) (Sir) Teall, J. J. H., “The Metamorphosis of Dolerite into Hornblendeschist”: Quart. Journ. Geol. Soc., xli, 1885, 133.CrossRefGoogle Scholar