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XXI.—The Tholeiites and Dolerites of the Dalmahoy Syncline

Published online by Cambridge University Press:  06 July 2012

Extract

The shallow synclinal fold termed the Dalmahoy syncline is situated between the north-western flank of the Pentland Hills and the Murieston fault, the most southerly of the five important easterly and north-easterly dislocations which traverse the oil-shale field of West Lothian. The core of the syncline is occupied by rocks belonging to the lower division of the Oil-Shale Group of the Lower Carboniferous. Intervening between these and the Cement-stone Group is a volcanic zone, probably on the same horizon as the Arthur's Seat lavas, consisting mainly of mugearites and basalts which show their greatest development in the Corston Hill district. Along the whole of the southern limb of the syncline is an extensive spread of Upper Old Red Sandstone, but this formation is almost entirely cut out in the northern limb by the Murieston fault, appearing only in the core of a small anticline near Selms.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1927

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References

page 489 note * Essai Géologique sur L'Écosse, (circa 1820), pp. 127 and 157.

page 489 note † A Description of the Western Isles of Scotland, 1819, vol. i, p. 504Google Scholar.

page 489 note ‡ Geology of Fife and the Lothians, 1st ed., 1839, pp. 171173Google Scholar; and 2nd ed., 1866, pp. 234–236.

page 490 note * Quart. Journ. Geol. Soc., 1874, vol. xxx, p. 555Google Scholar.

page 490 note † Trans. Roy. Soc. Edin., 1879, vol. xxix, p. 517Google Scholar.

page 490 note ‡ British Petrography, 1888, p. 190.

page 490 note § “The Neighbourhood of Edinburgh,” Mem. Geol. Surv. Scotland, 1910, p. 291.

page 490 note ∥ Trans. Edin. Geol. Soc., 1920, vol. xi, pp. 1617Google Scholar.

page 490 note ¶ Ibid., 1920, vol. xi, pp. 51–53 and 128–130.

page 490 note ** Min. Mag., vol. xx, 1925, p. 435440Google Scholar.

page 493 note * Loc. cit., p. 439.

page 493 note † Trans. Edin. Geol. Soc., 1920, vol. xi, p. 17Google Scholar.

page 493 note ‡ Geology of Fife and the Lothians, 1st ed., 1839, p. 171Google Scholar; and 2nd ed., 1866, p. 234.

page 493 note § “The Neighbourhood of Edinburgh,” Mem. Geol. Surv. Scotland, 1910, pp. 314 and 315.

page 493 note ∥ Trans. Edin. Geol. Soc., 1920, vol. xi, pt. i, pp. 5153Google Scholar; and 1923, vol. xi, pt. ii, pp. 128–130.

page 494 note * Information obtained from records in Geological Survey Office, Edinburgh.

page 494 note † Geological Survey 6-inch Map, Edinburghshire, Sheet 5, S.E.

page 495 note * “The Geology of the Neighbourhood of Edinburgh,” Mem. Geol. Surv., 1910, p. 292.

page 495 note † Tertiary and Post-Tertiary Geology of Mull,” ibid., 1924, p. 280.

page 495 note ‡ Op. cit., p. 303.

page 497 note * Quart. Journ. Geol. Soc., vol. xxx, 1874, p. 549, and pl. xxxiv, fig. 28Google Scholar.

page 497 note † British Petrography, 1888, p. 212, and pl. xxiii, fig. 2.

page 498 note * Min. Mag., vol. xx, 1925, p. 436Google Scholar.

page 498 note † Characteristics of Volcanoes, 1890, pp. 324–326.

page 498 note ‡ “Uber die Mineralbildung in Silikatschmelzlösungen,” Videnskabs-Selskabets Skrifter. I. Math.-naturv. Klasse., 1903, p. 112.

page 500 note * Quart. Journ. Geol. Soc., vol. liii, 1897, p. 487Google Scholar.

page 500 note † Compare Wadia, D. N., “Palagonite-bearing Dolerite from Nagpur,” Rec. Geol. Surv., India, vol. lviii, 1925, p. 342Google Scholar; and L. L. Fermor, “On the Basaltic Lavas penetrated by the deep boring for Coal at Bhusawal, Bombay Presidency,” ibid., p. 133.

page 500 note ‡ The Basalt of Bolshezemelsck tundra,” Trav. Musée Géol. Pierre le Orand, Acad. Sci. St Pétersburg, vol. iv, 1911, pp. 7597Google Scholar.

page 500 note § Min. Mag., vol. xxi, 1926, pp. 7382Google Scholar.

page 500 note ∥ Washington, H. S., “Chemical Analyses of Igneous Rocks,” U.S. Geol. Surv., Prof. Paper, 99, 1917, p. 888Google Scholar.

page 501 note * Op. cit., Mem. Geol. Surv., 1908, pp. 130–131.

page 501 note † “Tertiary and Post-Tertiary Geology of Mull,” ibid., 1924, p. 26.

page 503 note * “Tertiary and Post-Tertiary Geology of Mull,” Mem. Geol. Surv., 1924, p. 19.

page 503 note † “The Neighbourhood of Edinburgh,” ibid., 1910, pp. 298 and 307.

page 503 note ‡ Ibid., 1910, pp. 292–3.