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Chemical correlation of Moinian rocks in the northern Highlands of Scotland

Published online by Cambridge University Press:  01 May 2009

J. A. Winchester
Affiliation:
Department of Geology, University of Keele, Keele, Staffs, England ST5 5BG
R. St J. Lambert
Affiliation:
Department of Geology, University of Alberta, Edmonton, Alberta, CanadaT6G 2E3
J. G. Holland
Affiliation:
Department of Geological Sciences, Science Laboratories, South Road, Durham, England DHI 3LE

Summary

Comparison is made between the semipelitic and psammitic schists of the Morar and Glenfinnan Division in their type areas and the succession in the Fannich district of Northern Ross-shire. The tentative lithological correlation of the Morar Pelite with the Sgurr Mor Pelite is confirmed, while the Meall an t-Sithe Pelite and the semipelites of the Glenfinnan Division likewise have a similar geochemistry. In establishing these similarities, ratios involving Sr, Nb, Y, Zr and P2O5 have been found to be most useful, particularly Sr/Y. Other ratios (Ca/Y, K/Rb, K2O/(Na2O+CaO) and K/Ba) can also yield useful information regarding correlation and sedimentary history. Sr/Y decreases stratigraphically upwards in these successions and also towards the north east, suggesting a palaeogeography for the Morar Division involving increasing remoteness from the source area with time and in a northeasterly direction.

Type
Articles
Copyright
Copyright © Cambridge University Press 1983

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References

REFERENCES

Butler, B. C. M. 1965. A chemical study of some rocks of the Moine Series of Scotland. Q. Jl geol. Soc. Lond. 121, 163208.Google Scholar
Fleuty, M. J. 1962. The three fold-systems in the metamorphic rocks of upper Glen Orrin, Ross-shire and Inverness-shire. J. Geol. Soc. Lond. 117, 447–76.Google Scholar
Johnstone, G. S., Smith, D. I. & Harris, A. L. 1969. The Moinian Asemblage of Scotland. Mem. Am Ass. Petrol. Geol. 12, 159–80.Google Scholar
Lambert, R. St J., Winchester, J. A. & Holland, J. G. 1981. Comparative geochemistry of pelites from the Moinian and Appin Group (Dalradian) of Scotland. Geol. Mag. 118, 477–90.Google Scholar
Lambert, R. St J. & Poole, A. B. 1964. The relationship of the Moine Schists and Lewisian gneisses near Mallaigmore, Inverness-shire. Proc. Geol. Ass. Lond. 75, 114.Google Scholar
Peach, B. N., Gunn, W., Horne, J., Clough, C. T. & Greenly, E. 1913. The geology of the Fannich Mountains and the country around upper Loch Maree and Strath Broom. Mem. geol. Surv. Sheet 92.Google Scholar
Poole, A. B. 1966. The stratigraphy and structure of north-eastern Morar, Inverness-shire. Scott. J. Geol. 2, 3853.CrossRefGoogle Scholar
Powell, D. 1964. The stratigraphical succession of the Moine Schists around Lochailort (Invernessshire) and its regional significance. Proc. Geol. Ass. Lond. 75, 223250.CrossRefGoogle Scholar
Powell, D. 1974. Stratigraphy and structure of the western Moine and the problem of Moine orogenesis. J. geol. Soc. Lond. 130, 575–93.Google Scholar
Powell, D., Baird, A. W., Charnley, N. R. & Jordan, P. J. 1981. The metamorphic environment of the Sgurr Beag Slide: a major crustal displacement zone in Proterozoic Moine rocks of Scotland. J. geol Soc. Lond. 138, 661–73.Google Scholar
Ramsay, J. G. 1957(a). Superimposed folding at Loch Morar, Inverness-shire and Ross-shire. Q. Ji geol. Soc. Lond. 113, 271307.Google Scholar
Ramsay, J. G. 1957(b). Moine-Lewisian relations of Glenelg, Inverness-shire. Q. Jl geol. Soc. Lond. 113, 487523.CrossRefGoogle Scholar
Ramsay, J. G. & Spring, J. S. 1962. Moine stratigraphy in the western Highlands of Scotland. Proc. Geol. Ass. Lond. 73, 295322.Google Scholar
Rathbone, P. A. & Harris, A. L. 1979. Basement-cover relationships at Lewisian inliers in the Moine rocks. In The Caledonides of the British Isles - reviewed (ed. Harris, A. L., Holland, C. H. and Leake, B. E.). Spec. Publ. geol. Soc. Lond. 8, 101–7.Google Scholar
Richey, J. E. & Kennedy, W. Q. 1939. The Moine and sub-Moine series of Morar, Inverness-shire. Bull. geol. Surv. Gt Brit. 2, 2645.Google Scholar
Tanner, P. W. G. 1970. The Sgurr Beag Slide - a major tectonic break within the Moinian of the Western Highlands of Scotland. Q. Jl geot. Soc. Lond. 126, 435–63.Google Scholar
Tanner, P. W. G., Johnstone, G. S., Smith, D. I. & Harris, A. L. 1970. Moinian stratigraphy and the problem of the Central Ross-shire Inliers. Bull. geol. Soc. Am. 81, 299306.Google Scholar
Tobisch, O. T., Fleuty, M. J., Merh, S. S., Mukhopadhyay, D. & Ramsay, J. G. 1970. Deformational and metamorphic history of Moinian and Lewisian rocks between Strath Conon and Glen Affric. Scott. J. Geol. 6, 243–65.CrossRefGoogle Scholar
Winchester, J. A. 1973. Extensions to the Lewisian Inliers of Fannich Forest, Ross-shire. Proc. Geol. Ass. 84, 273–82.Google Scholar
Winchester, J. A., Lambert, R. St J. & Holland, J. G. 1981. Geochemistry of the western part of the Moinian assemblage. Scott. J. Geol. 17, 281–94.CrossRefGoogle Scholar