Published online by Cambridge University Press: 01 May 2009
Almost all the more important teschenitic intrusions of the Edinburgh district have been examined in some detail at one time or another, but the large sill situated between Dunfermline and Charlestown is a notable exception. In the course of an investigation last autumn, the writer found, however, that, while the normal rock is not specially noteworthy, its segregations present some interesting features, particularly in view of a recent publication by Dr. G. W. Tyrrell dealing with the age and classification of the analcitic intrusions of Central Scotland.
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page 344 note 2 Geology of the Edinburgh District, 1910, p. 293.Google Scholar
page 344 note 3 Trans. Roy. Soc. Edin., vol. liii, part 2, p. 372.Google Scholar
page 345 note 1 Geol. Mag., Vol. LIX, 1922, p. 450.Google Scholar
page 346 note 1 Loc. cit.Google Scholar
page 346 note 2 Geol. Mag., Vol. LX, 1923, pp. 530–42.Google Scholar
page 346 note 3 Loc. cit., pp. 250, 251.Google Scholar
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page 347 note 1 Compare Edinburgh Memoir, pl. xi, fig. 4, with Geol. Mag., 1923, Pl. XI, Fig. 4.Google Scholar
page 347 note 2 Mem. Geol. Surv. Scotland, Glasgow District, 1911, p. 113.Google Scholar