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H. G. Backlund classifies basalts as 1. Plateau-basalts; 2. Geosynical basalts. These classes correspond closely to those given above.Zur genetischen Deutung der Eklogite. Geol. Rundsch. 2, 1936, p. 49.
A comprehensive discussion of the ophiolitic suite is given byG. Steinmann,Die ophiolitischen Zonen in den mediterränen Kettengebirge, Congr. Geol. Internat. XIV Session Madrid, 1926, Fasc. 2. pp. 637-67.
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The Scottish sub-region is dealth with in the following memoirs of the Geological Survey of Scotland (abbreviated titles): ≪Tertiary Igneous Rocks of Skye, 1904;Geology of the Small Isles, 1908;Geology of Mull, 1924;Geology of Arran, 1928;Geology of Ardnamurchan ≫, 1930.
See,G. W. Tyrrell,The Geology of Arran Mem. Geol. Surv. Scotland, 1928;F. Walker,Differentiation in the Sills of Northern Trotternish (Skye), Trans. Roy. Soc. Edin., LVII, Pt. I. 1932, 241-57;F. Walker andC. F. Davidson.A Contribution to the Geology of The Faröes, ibid., LVIII, Pt. III, 1936, pp. 869-97.
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SirA. Geikie,Textbook of Geology 4th edition, 1903, p. 264.
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H. T. Stearns andW. O. Clark, op. cit., p. 65.
H. T. Stearns andW. O. Clark, op. cit., p. 77, 130 et seq.
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H. T. Stearns, inGeology and Ground-water Resources of the Island of Oahu, Hawaii. Territory of Hawaii, Division of Hydrography, Bull. 1, 1935, pp. 20, 95.
For an excellent general account of this region see,J. F. Richey Tertiary Ring Structures in Britain, Trans. Geol. Soc. Glasgow, XIX pt. 1, 1932, pp. 42–140; and British Regional Geology: Scotland:The Tertiary Volcanic Districts, Geol. Surv. 1935, 115 pp.
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Op. cit. supra, pp. 48-9.
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Op, cit. supra, pp. 138-40.
Mull Memoir, 1924, pp. 131 et seq., 173, 179, 339 et seq.
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Paper delivered at the Section of Volcanology, International Union of Geodesy and Geophysics, Edinburgh, Sept. 22, 1936).
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Tyrell, G.W. Flood basalts and fissure eruption. Bull Volcanol 1, 89–111 (1937). https://doi.org/10.1007/BF03028044
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DOI: https://doi.org/10.1007/BF03028044