Hostname: page-component-cd9895bd7-p9bg8 Total loading time: 0 Render date: 2024-12-26T07:20:21.840Z Has data issue: false hasContentIssue false

Some Structures in the Dalradian Pillow Lavas of the Tayvallich Peninsula, Argyll

Published online by Cambridge University Press:  01 May 2009

Dennis S. Wood
Affiliation:
Department of Geology, The University, Leeds, 2.

Abstract

Pillows are described in various stages of production from small parent lava flows. The lavas flowed into water–laden sediments down to depths at which the latter were capable of supporting the weight of lava. Because of their lack of systematic relationship to tectonic axes, certain structures observed in these sediments are interpreted as pushing folds induced by the “intrusion” of lava flows. The direction of flow of the lavas was towards the north.

Type
Articles
Copyright
Copyright © Cambridge University Press 1964

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

REFERENCES

Anderson, T., 1910. The Volcano of Matavanu in Savaii. Quart. J. geol. Soc. Lond., 66, 621639.CrossRefGoogle Scholar
Benson, W. N., 1915. The Geology and Petrology of the Great Serpentine Belt of New South Wales. Proc. Linn. Soc. N.S. Wales, 40, 121173.CrossRefGoogle Scholar
Dewey, H. and Flett, J. S., 1911. On Some British Pillow Lavas and the Rocks Associated With Them. Geol. Mag. (5) 8, 202209, 241–248.CrossRefGoogle Scholar
Fox, H. and Teall, J. J. H., 1893. On a Radiolarian Chert from Mullion Island. Quart. J. geol. Soc. Lond., 49, 211220.CrossRefGoogle Scholar
Geikie, Sir A., 1897. Ancient Volcanoes of Great Britain. London.CrossRefGoogle Scholar
Geikie, Sir A., 1900. The Geology of Central and Western Fife. Mem. geol. Surv. U.KGoogle Scholar
Geikie, Sir A., 1903. Textbook of Geology, 4th ed., LondonGoogle Scholar
Gilluly, J., 1935. Keratophyres of Eastern Oregon and the Spilite Problem. Amer. J. Sci., 29, 225252, 336–352.CrossRefGoogle Scholar
Greenly, E., 1902. The Origins and Associations of the Jasper of Southeastern Anglesey. Quart. J. geol. Soc. Lond., 58, 425440.CrossRefGoogle Scholar
Greenly, E., 1919. The Geology of Anglesey. Mem. geol. Surv. U.K.Google Scholar
Harker, A., 1909. The Natural History of Igneous Rocks. New York.Google Scholar
Lewis, J. V., 1914. Origin of Pillow Lavas. Bull. geol. Soc. Amer., 25, 591654.CrossRefGoogle Scholar
Naumann, , 1834. Erläuterungen zur geognotische Karte des Konigreichs Sachsen. Pt. 1.Google Scholar
Peach, B. N., 1904. Sum. Prog. geol. Surv. U.K. for 1903, 69.Google Scholar
Peach, B. N., 1911. In The Geology of Knapdale, Jura and North Kintyre. Mem. geol. Surv. U.K., 28.Google Scholar
Plantania, G. and Johnston-Lavis, H. J., 1891. The South Italian Volcanoes. Naples.Google Scholar
Reid, C. and Dewey, H., 1908. The Origin of Pillow Lava Near Port Isaac, in Cornwall. Quart. J. geol. Soc. Lond., 64, 264272.CrossRefGoogle Scholar
Stearns, H. T., 1937. Pillow Lavas in Hawaii (abs.). Geol. Soc. Amer. Proc. for 1937, 252.Google Scholar
Tromp, S. W., 1937. On the Mechanism of the Geological Undulation Phenomena. Leiden.Google Scholar
Vuagnat, M., 1949. Sur les Pillow Lavas Dalradiennes de la Peninsule de Tayvallich (Argyllshire). Schweiz. Min. Petr. Mitt., 29, 523536.Google Scholar
Whitley, N., 1849. On the Remains of Ancient Volcanoes on the North Coast of Cornwall in the Parish of St. Minver. 30th Ann. Rept. Roy. Inst. Cornwall, App. 6.Google Scholar