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Evidence for the Geological Dating of the Granitic Gneiss of Western Ardgour

Published online by Cambridge University Press:  01 May 2009

I. W. D. Dalziel  and
M. R. W. Johnson
I. W. D. Dalziel
Affiliation:
Grant Institute of Geology, West Mains Road, Edinburgh.
M. R. W. Johnson
Affiliation:
Grant Institute of Geology, West Mains Road, Edinburgh.
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Abstract

Evidence is presented for the geological dating of the granitic gneiss of western Ardgour, the southernmost part of the discontinuous granitic gneiss outcrop which extends from Argyll to Inverness-shire along the Loch Quoich line between the “highly inclined” and “flat” belts of the Moines. The granitic gneiss is shown to have been formed before or early in the second of four main fold movements to which the surrounding metasediments have been subjected, and is thought to occupy the core of a complex anti-formal second major fold.

Type
Articles
Information
Geological Magazine , Volume 100 , Issue 3 , June 1963 , pp. 244 - 254
Copyright
Copyright © Cambridge University Press 1963

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References

REFERENCES

Bailey, E. B. and Maufe, H. B., 1916. The Geology of Ben Nevis and Glencoe. Mem. geol. Surv. U.K.Google Scholar
Clifford, T. N., 1957. The Stratigraphy and Structure of part of the Kintail District of Southern Ross-shire: its Relation to the Northern Highlands. Quart. J. geol. Soc. Lond., 113, 57–85.CrossRefGoogle Scholar
De Sitter, L. U., 1958. Boudins and Parasitic Folds in Relation to Cleavage and Folding. Geol. en Mijnb., 20, 277–286.Google Scholar
Haller, J., 1956. Problems der Tiefentektonik Bauformen in Migmatit-Stockwerk der Ostgrönländischen Kaledoniden. Geol. Rdsch., 45, 159–167.CrossRefGoogle Scholar
Harry, W. T., 1953. The Composite Granitic Gneiss of Western Ardgour, Argyll. Quart. J. geol. Soc. Lond., 109, 285–308.Google Scholar
Lawrie, T. R. M., Johnstone, G. S. and Wright, J. E., 1953–1957. Scottish Highlands and Islands. Summ. Progr. geol. Surv. G.B., for 1951–1956.Google Scholar
Leedal, G. P., 1952. The Cluanie Igneous Intrusion, Inverness-shire and Ross-shire. Quart. J. geol. Soc. Lond., 108, 35–62.CrossRefGoogle Scholar
Peach, B. N. and Wilson, J. S. G., 1904. West Highland District. Summ. Progr. geol. Surv. G.B., for 1903, p. 68.Google Scholar
Phemister, J., 1960. British Regional Geology. Scotland: The Northern Highlands. 3rd Edition. H.M.S.O. Edinb.Google Scholar
Ramberg, H., 1956. Pegmatites in West Greenland. Bull. geol. Soc. Amer., 67, 185–213.Google Scholar
Ramsay, J. G., 1958. Superimposed Folding at Loch Monar, Inverness-shire and Ross-shire. Quart. J. geol. Soc. Lond., 113, 271–305.CrossRefGoogle Scholar
Read, H. H., 1961. Aspects of Caledonian Magmatism in Britain. Lpool. Manchr. geol. Journ., 2, 653–683.CrossRefGoogle Scholar
Richey, J. E. and Kennedy, W. Q., 1939. The Moine and Sub-Moine Series of Morar, Inverness-shire. Bull. geol. Surv. G.B., 2, 26–45.Google Scholar
Wegmann, C. E., 1935. Zur Deutung der Migmatite. Geol. Rdsch., 26, 305–350.CrossRefGoogle Scholar