Published online by Cambridge University Press: 01 May 2009
The object of this paper is to give a connected account of the small plutonic masses which pierce the Lower Palaeozoic strata of South-East Scotland. These intrusions have been overshadowed by their larger neighbours the Galloway Granites, of which Teall has given such admirable descriptions, but are worthy of more attention than they have received in the past.
page 153 note 1 “Silurian Rocks of Great Britain”: Mem. Geol. Surv., pt. i, Scotland, 1899, pp. 607–25.Google Scholar
page 153 note 2 Illustrations, p. 328.
page 153 note 3 Essai Geologique sur l'Ecosse, p. 94.
page 153 note 4 Mineralogy of Dumfries, Appendix.
page 153 note 5 Mem. Geol. Surv., Lothian, E., 1st ed., pp. 15–17.Google Scholar
page 153 note 6 Trans. Roy. Soc. Edin., vol. xvi, p. 39.Google Scholar
page 153 note 7 Mem. Geol. Surv., E., Berwickshire, 1864, p. 29.Google Scholar
page 153 note 8 “Silurian Rocks of Great Britain”: Mem. Geol. Surv., pt. i, Scotland, 1899, p. 625; E. Lothian, 2nd ed., 1911, p. 22.Google Scholar
page 154 note 1 Op. cit., p. 625.
page 154 note 2 Trans. glasgow Geol. Soc., vol. x, p. 256.Google Scholar
page 154 note 3 op. cit., p. 27.
page 154 note 4 op. cit., p. 40.
page 154 note 5 Trans. Edin. Geol. Soc., vol. xi, pt. iii, pp. 357–65.Google Scholar
page 156 note 1 The above names are used in accordance with the recommendations of the Committee on British Petrographic Nomenclature, vide Mineralogical Magazine, vol. xix, No. 92, p. 137.Google Scholar
page 159 note 1 Cf. Sir John Flett, GE0L. MAG., 1898, p. 388.
page 159 note 2 op. cit., p. 363.
page 160 note 1 Amer. Journal Sri., 1914, p. 257.Google Scholar