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Element Distribution in Two Epidiorite Sills from the Central Grampian Highlands of Scotland

Published online by Cambridge University Press:  01 May 2009

T. K. Ball
T. K. Ball
Affiliation:
Building Research Station, Garston, Watford, Herts.
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Abstract

Magmatic differentiation is demonstrated in two epidiorite sills from the Grampian Highlands of Scotland, and the distribution of major and minor elements compared with data given for other intrusions, and for trace elements in the Whin Sill at High Cup Gill, Westmorland. The latter sill has Sr and Ba enriched towards the top. The element distribution for the epidiorite sills indicates that they are overturned. The data are conclusive for one sill but merely suggestive for the other, since such phenomena as multiple injection may also have affected the element distribution. The structural significance is briefly discussed.

Type
Articles
Information
Geological Magazine , Volume 102 , Issue 2 , April 1965 , pp. 93 - 105
Copyright
Copyright © Cambridge University Press 1965

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References

REFERENCES

Bailey, E. B., 1922. The structure of the South-west Highlands of Scotland. Quart. J. geol. Soc. Lond., 79, 423.Google Scholar
Bayley, R. W., 1959. A metamorphosed differentiated sill in Northern Michigan. Amer. J. Sci., 257, 408–430.CrossRefGoogle Scholar
Borisenko, L. F., 1959. On the distribution of Sc in igneous rocks on the example of some massifs of the Soviet Union. Geochemistry (Geokhimya), 7, 770–778.Google Scholar
Bowes, D. R., and Jones, K. A., 1958. Sedimentary features and tectonics in the Dalradian of Western Perthshire. Trans. Edin. geol. Soc., 17, 133–140.CrossRefGoogle Scholar
Campbell, R., Day, T. C., and Stenhouse, A. G., 1933. The Braefoot Outer Sill, Fife. Part II. Trans. Edin. geol. Soc., 23, 148–173.Google Scholar
Carr, M. M., and Turekian, K. K., 1961. The geochemistry of cobalt. Geochim. et Cosmochim. Acta, 23, 9–60.CrossRefGoogle Scholar
Goldschmidt, V. M., 1954. Geochemistry. Oxford University Press.Google Scholar
Green, J., 1959. Geochemical table of the elements for 1959. Bull. geol. Soc. Amer., 70, 1127–1184.CrossRefGoogle Scholar
Grubenmann, U., 1910. Die Kristallinen Schiefer. Berlin.Google Scholar
Heier, K. S., 1960. Petrology and geochemistry of high-grade metamorphic rocks on Langøy, Northern Norway. Norges Geol. Unders., 207.Google Scholar
Higazy, R. A., 1952. The distribution and significance of the trace elements in the Braefoot Outer Sill, Fife. Trans. Edin. geol. Soc., 15, 150–186.CrossRefGoogle Scholar
Jones, K. A., 1960. Origin of albite porphyroblasts in rocks of the Ben Mo- Am Binnein area, Western Perthshire, Scotland. Geol. Mag., 48, 41–55.Google Scholar
Jones, K. A., 1962. Metamorphism of the Ben More-Am Binnein area, Western Perthshire. Proc. geol. Soc. Lond., No. 1600, 121–125.Google Scholar
Lundegardh, P. H., 1947. Rock composition and development in Central Roslagen, Sweden. Arkiv Kemi, Min. Geol., 23A, 1–160.Google Scholar
Neumann, H., 1961. The scandium content of some Norwegian minerals and the formation of thorveitite; a reconnaissance survey. Norsk Geol. Tidsskr., 41, 197–210.Google Scholar
Nockolds, S. R., and Allen, R., 1954–1956. The geochemistry of some igneous rock series, Parts 1–3: Geochim. et Cosmochim. Acta, 4, 105–142; 5, 245–285; 9, 34–57.CrossRefGoogle Scholar
Nockolds, S. R., and Mitchell, R. L., 1948. The geochemistry of some Caledonian Plutonic rocks. Trans. Roy. Soc. Edin., 61, 533–575.CrossRefGoogle Scholar
Pantin, H. M., 1956. The petrology of the Ben Vrackie epidiorites and their contact rocks. Trans. geol. Soc. Glasgow, 22, 48–79.CrossRefGoogle Scholar
Rankama, K., and Sahama, Th. G., 1950. Geochemistry. University of Chicago Press.Google Scholar
Rast, N., 1958. The metamorphic history of the Schichallion Complex. Trans. Roy. Soc. Edin., 63.CrossRefGoogle Scholar
Ringwood, A. E., 1955. The principles governing trace element distribution during magmatic crystallization. 1.—The influence of electro-negativity. Geochim. et Cosmochin. Acta, 7, 189–202.CrossRefGoogle Scholar
Sandell, E. B., and Goldich, S. S., 1943. The rarer metallic constituents of some American igneous rocks. J. Geol., 51, 99–115; 167–189.CrossRefGoogle Scholar
Storm, T. W., and Holland, H. D., 1957. Distribution of nickel in the Lambertville Diabase. Geochim. et Cosmochim. Acta, 11, 335–344.CrossRefGoogle Scholar
Sturt, B. A., and Harris, A. L., 1961. The metamorphic history of the Loch Tummel area, Central Perthshire, Scotland. Liv. and Man. Geol. Journ., 2, 689–711.Google Scholar
Taylor, S. R., 1955. The origin of some New Zealand metamorphic rocks as shown by their major and trace element abundances. Geochim. et Cosmochim. Acta, 8, 182–197.CrossRefGoogle Scholar
Turekian, K. K., 1956. The abundance of Cu, Ni, and Cr in basaltic rocks. Trans. Amer. Geophys. Un., 37, 361.Google Scholar
Turekian, K. K., and Kulp, J. L., 1956. The geochemistry of strontium. Geochim. et Cosmochin. Acta, 10, 245–266.CrossRefGoogle Scholar
Voll, G., 1960. New work on petrofabrics. Liv. and Man. geol. Journ., 2, 503–597.Google Scholar
Wager, L. R., 1960. The major element variation of the layered series of the Skaergaard Intrusion and a re-estimation of the average composition of the hidden layered series and of the successive residual magmas. J. Petrol., 1, 364–398.CrossRefGoogle Scholar
Wager, L. R., and Mitchell, R. L., 1951. The distribution of trace elements during strong fractionation of basic magma—a further study of the Skaergaard intrusion, East Greenland. Geochim. et Cosmochim. Acta, 1, 129–208.CrossRefGoogle Scholar