Published online by Cambridge University Press: 14 March 2018
The Permo-Carboniferous quartz-dolerites of central Scotland are generally holocrystalline, and only two intrusions amongst them with a fresh vitreous base have been recorded—those of Dalmeny in West Lothian, andKinkellnear Kirkintilloch (northof Glasgow). Both rocks have already been described briefly, but in view of their many interesting features a more thorough treatment seems desirable, particularly as they have a bearing on some recent theories of magmatie differentiation advanced by Dr. C. N. Fenner.
page 368 note 1 Mem. Geol. Survey, Edinburgh District, 1910, p. 306.
page 369 note 1 Since the above was written a paper by Dr. M. A. Peacock (Geol. Mag., 1930, vol. 67, p. 177) has appeared, in which he demonstrates the existence of two separate varieties of ehlorophaeite—a green and a brown. Both varieties seem to be present here.
page 371 note 1 A. V. Lothian, The petrology of the Kilsyth Hills. Privately printed, 1902, p. 15.
page 371 note 2 Bailey, E. B., Mem. Geol. Survey, Glasgow District, 1911, p. 146 Google Scholar.
page 374 note 1 C. N., Fenner, The crystallization of basalts. Amer. Journ. Sci., 1929, ser. 5, vol. 18, pp. 225–253.Google Scholar
page 374 note 2 C. N. Fenner, loc. cir., p. 242.
page 374 note 3 Washington, H. S., Bull. Geol. Soe. Amer., 1922, Vol. 33, p. 774.Google Scholar
page 374 note 4 H. S. Washington, loc. cit., p. 779.
page 375 note 1 Tilley, C. E., Min. Mag., 1922, vol. 19, p. 279.CrossRefGoogle Scholar
page 375 note 2 Walker, F. and Irving, J., Trans. Roy. Soc. Edinburgh, 1928, vol. 56, p. 12.Google Scholar
page 375 note 3 E. B. Bailey, loc. cit., p. 147.