Hostname: page-component-7479d7b7d-rvbq7 Total loading time: 0 Render date: 2024-07-12T19:06:26.441Z Has data issue: false hasContentIssue false

The Cairnsmore of Fleet Granite and its Metamorphic Aureole

Published online by Cambridge University Press:  01 May 2009

Extract

The Cairnsmore of Fleet granite is the second in point of size of the four plutonic masses which penetrate the Lower Palaeozoic rocks of the Southern Uplands of Scotland, being exceeded in area only by that of the Criffel. Its outline is roughly oval and it measures 11 miles by 7 miles, the long axis trending N.E.—S.W., exactly parallel to the strike of the rocks of the Southern Uplands.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1937

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

Works to which Reference is made

Allport, S., and Bonney, T. G., 1889. “Report on the Effects of Contact Metamorphism exhibited by the Silurian Rocks near New Galloway, in the Southern Uplands of Scotland,” Proc. Boy. Soc., xlvi, 193204.Google Scholar
Deer, W. A., 1935. “The Cairnsmore of Carsphairn Igneous Complex,” Quart. Journ. Geol. Soc., xci, 4774.Google Scholar
Gardiner, C. I., and Reynolds, S. H., 1932. “The Loch Doon “Granite” Area, Galloway,” Quart. Journ. Geol. Soc., lxxxviii, 134.CrossRefGoogle Scholar
Gardiner, M. I., 1890. “Contact Alteration near New Galloway,” Quart. Journ. Geol. Soc., xlvi, 569580.CrossRefGoogle Scholar
Geological Survey, 1924. Summary of Progress of the Geological Survey of Great Britain for 1923, p. 134. (Rock analyses of the Talnotry diorite by E. G. Radley.)Google Scholar
Gregory, J. W., 1927. “The Nickel-Cobalt Ore of Talnotry, Kirkcudbrightshire,” Trans. Inst. Min. Met., pp. 118.Google Scholar
Hall, Sir James, 1815. “On the Vertical Position and Convolutions of certain strata and their Relation with Granite,” Trans. Roy. Soc. Edinburgh, vii, 79108.CrossRefGoogle Scholar
Jones, O. T., 1924. “Lead and Zinc Ores in the Slaty Rocks of Britain,” Trans. Inst. Min. Eng., lxvi, 266.Google Scholar
Teall, J. J. H., 1899. In “The Silurian Rocks of Britain. Vol. I: Scotland,” Mem. Geol. Surv. U.K., chapters xxvi and xxvii, 607651.Google Scholar
Tilley, C. E., 1926. “On garnet in pelitic contact zones,” Min. Mag., xxi, 49.Google Scholar
Wilson, G. V., 1921. “Lead, Zinc, Copper, Nickel Ores of Scotland,” Mem. Geol. Surv. Scotland, xvii.Google Scholar