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VI.—The Chawfordjohn Essexite and Associated Rocks

Published online by Cambridge University Press:  01 May 2009

Extract

Although the so-called Crawfordjohn essexite has been mentioned several times in petrographic literature, no detailed description of the occurrence has been given. In 1888 Teall described the main rock of the intrusion as an abnormal variety ofthe N. W.-S.E. Kainozoic dykes and noted the porphyritic augite andthe abundance of felspar, olivine, and apatite. Lacroix, in a generalpaper on the teschenites, mentioned the occurrence of nephelite in the same rock, which he described as an “olivine-teschenite, passing instructure to a tephrite”. Bailey, in the Glasgow memoir, remarked on the close similarity between the Crawfordjohn and Lennoxtown rocks and classed them with the essexites on account of their chemical similarity to the Brandberget rocks, while Tyrrell, on account ofthis similarity and also of the resemblance to the Carclout essexite, included them in the late Palaeozoic alkaline group.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1915

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References

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page 458 note 1 Cf. Campbell, R. & Stenhouse, A. G., Trans. Edin. Geol. Soc., ix, p. 126, 1907.Google Scholar

page 458 note 2 Includes some turbid unidentified matter.

page 458 note 3 Includes a little hornblende.

page 458 note 4 Cf. Tyrrell, G. W., Geol. Mag. [5], IX, p. 121, 1912. The writer is indebted to Mr. Tyrrell for the loan of slides of this rock.Google Scholar

page 458 note 5 Ibid., p. 77.

page 458 note 6 Ibid., p. 123.

page 459 note 1 Cf.Flett, J. S.in Geology of Edinburgh(Mem. Geol. Surv.), 1910, p. 295.Google Scholar

page 459 note 2 Summary of Progress of Geological Survey for 1907, 1908, p. 55; E. B. Bailey, loc. cit., p. 130.

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page 459 note 7 Loc. cit.

page 460 note 1 Bull, . Essex Inst., xxiii, p. 146,1891.Google Scholar

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page 460 note 3 Loc. cit.

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