Hostname: page-component-cd9895bd7-dzt6s Total loading time: 0 Render date: 2024-12-26T19:38:58.201Z Has data issue: false hasContentIssue false

Differentiation in Basalt Lava, Island Magee, Co. Antrim

Published online by Cambridge University Press:  01 May 2009

Extract

THE plateau-lavas of Antrim cover an area of approximately 1,550 square miles—the largest area of Tertiary lavas in the British Isles. Although from the earliest daysof geological science these lavas have attracted many observers, very little has been done in the way of petrological study and, curiously enough, the dominant olivine-basalt lava has never been analysed.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1934

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

(1)The Tertiary and post-Tertiary geology of Mull, Loch Aline and Oban,” Mem. Geol. Survey, Scotland, 1924, 15.Google Scholar
(2) Ross, C. S. and Shannon, E. V., “The origin, occurrence, composition and physical properties of the mineral iddingsite,” Proc. U.S. Nat. Mus., lxvii, 1925, 1.CrossRefGoogle Scholar
(3) Hull, E., “Expl. Mem. Sheet 21, 28, and 29,” Geol. Survey Ireland, 1876, 30.Google Scholar
(4) Hardman, E. T.On hullite, a hitherto undescribed mineral; a hydrous silicate of peculiar composition from Carnmoney Hill, Co. Antrim, with analysis. With notes on the microscopical appearances by Professor Hull, F.R.S.,” Proc. R. Irish Acad., 2, iii, 1878, 161.Google Scholar
(5) Lacroix, A.Sur le kirwanite et le hullite,” Bull. Soc. Min. France, viii, 1885, 432.Google Scholar
(6) Cole, G. A. J.Hullite,” Proc. Belfast Nat. Field Club, 2, iv, 18941895, 221.Google Scholar
(7) Heddle, M. F.Chapters on the mineralogy of Scotland. VI. Chloritic minerals,” Tr. R. Soc. Edinburgh, xxix, 1880, 55.Google Scholar
(8) Sollas, W. J., and McHenry, A.On a volcanic neck of Tertiary age in the County of Galway,” Trans. R. Irish Acad., xxx, 1896, 729.Google Scholar
(9) Vogt, J. H. L.The physical chemistry of the crystallization and magmatic differentiation of igneous rocks,” Journ. Geol., xix, 1921, 524527.Google Scholar
(10) Walker, F.The geology of the Shiant Isles (Hebrides),” Quart. Journ. Geol. Soc., lxxxvi, 1930, 377.Google Scholar
(11) Daly, R. A.Magmatic differentiation in Hawaii,” Journ. Geol., xix, 1911, 295.Google Scholar
(12) Quensel, P. D.Die Geologie der Juan Fernandezinseln,” Bull. Geol. Inst. Upsala, xi, 1912, 252.Google Scholar
(13) Bowen, N. L.The Evolution of the Igneous Rocks, Princeton, 1928, 159164.Google Scholar
(14) Kennedy, W. Q.Trends of differentiation in basaltic magmas,” Am. Journ Sci., xxv, 1933, 239.CrossRefGoogle Scholar
(15) Harker, A.The Tertiary igneous rocks of Skye,” Mem. Geol. Survey, 1904.Google Scholar
(16) Strachan, J.The origin and formation of zeolites in basalt,” Proc. Belfast Nat. Field Club, 2, vi, 19071908, 92.Google Scholar
(17) Fenner, C. N.The Watchung basalt and the paragenesis of its zeolites and other secondary minerals,” Ann. N.Y. Acad. Sci., xx, 1910, 93.Google Scholar
(18) McLintock, W. F. P.On the zeolites and associated minerals from the Tertiary lavas around Ben More, Mull,” Tr. R. Soc. Edinburgh, li, 1915, 1.Google Scholar
(19) Holmes, A.The Tertiary volcanic rocks of Mozambique,” Quart. Journ. Geol. Soc., lxxii, 1916, 222.CrossRefGoogle Scholar