Hostname: page-component-76fb5796d-5g6vh Total loading time: 0 Render date: 2024-04-26T01:41:58.796Z Has data issue: false hasContentIssue false

Precambrian and Palaeozoic rocks of the Inner Hebrides

Published online by Cambridge University Press:  26 July 2012

R. Anderton
Affiliation:
Department of Applied Geology, University of Strathclyde, Glasgow Gl 1XJ
D. R. Bowes
Affiliation:
Department of Geology, University of Glasgow, Glasgow G12 8QQ
Get access

Synopsis

The Lewisian complex, which forms the continental basement to north-west Scotland, crops out on the Inner Hebridean islands of Rona, Raasay, Skye, Coll, Tiree, Iona and Islay. Upon this basement, four major rock successions were deposited before the Caledonian orogeny. The upper Precambrian Moine assemblage forms only a small area of metamorphosed rocks on Mull but the c. 790 m.y. (million year) old Torridonian sediments are found on Raasay, Scalpay. the Sleat of Skye, Soay and Rhum. The upper Precambrian to Cambrian Dal radian Supergroup dominates Islay, Jura, Gigha and the islands of the Firth of Lome whilst also forming a partial rim around the Tertiary Northern granite in Arran. Other Precambrian rocks of uncertain affinity are found on Islay, Oronsay, Colonsay and Iona. Cambro-Ordovician sediments are found on Skye where they have been partially metamorphosed by Tertiary intrusions.

South-east of the Moine thrust zone, the Precambrian and lower Palaeozoic rocks were deformed and metamorphosed during the late Cambrian to early Devonian Caledonian orogeny which resulted in the development of the Caledonian mountain chain. Subsequently, Scotland north-west of the Highland Boundary fault has tended to persist as a land area undergoing erosion with sedimentation restricted to peripheral areas now preserved around the present coast. Upper Palaeozoic rocks are therefore only well represented on Arran although Old Red Sandstone (Devonian) sediments are found in the Firth of Lome and a very small area of possible Permian rocks occurs on Islay.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1983

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

Each reference to a paper in the Symposium carries an asterisk indicating that it is contained in Proc. Roy. Soc. Edinb. 83B.Google Scholar
Anderton, R. 1976. Tidal-shelf sedimentation: an example from the Scottish Dalradian. Sedimentology 23, 429–58.CrossRefGoogle Scholar
Anderton, R. 1982. Dalradian deposition and the late Precambrian-Cambrian history of the N Atlantic region: a review of the early evolution of the Iapetus Ocean. J. Geol. Soc. Lond. 139, 421431.CrossRefGoogle Scholar
Anderton, R. Bridges, P. H., Leeder, M. R. and Sellwood, B. W. 1979. A dynamic stratigraphy of the British Isles. London: George Allen & Unwin.Google Scholar
Barber, P. L., Dobson, M. R. and Whittington, R. 1979. The geology of the Firth of Lorne, as determined by seismic and dive sampling methods. Scott. J. Geol. 15, 217230.CrossRefGoogle Scholar
Bikerman, M., Bowes, D. R. and van Breemen, O. 1975. Rb-Sr whole rock isotopic studies of Lewisian metasediments and gneisses in the Loch Maree region, Ross-shire. J. Geol. Soc. Lond. 131, 237254.CrossRefGoogle Scholar
Bowes, D. R. 1968. The absolute time scale and the subdivision of Precambrain rocks in Scotland. Geol. För. Stockh. Förh. 90, 175188.CrossRefGoogle Scholar
Bowes, D. R. 1978. Shield formation in early Precambrian times: the Lewisian complex. In Crustal evolution in northwestern Britain and adjacent regions, ed. Bowes, D. R. and Leake, B. E. Geol. J. Spec. Issue 10, 39–80.Google Scholar
Bowes, D. R. Hopgood, A. M. and Pidgeon, R. T. 1976. Source ages of zircons in an Archaean quartzite, Rona, Inner Hebrides. Scotland. Geol. Mag. 113, 545552.CrossRefGoogle Scholar
Brewer, M. S., Brook, M. and Powell, D. 1979. Dating of the tectono-metamorphic history of the southwestern Moine, Scotland. In The Caledonides of the British Isles-reviewed, ed. Harris, A. L., Holland, C. H. and Leake, B. E. Spec. Publ. Geol. Soc. Lond. 8, 129–37.Google Scholar
Curry, G. B., Ingham, J. K., Bluck, B. J. and Williams, A. 1982. The significance of a reliable Ordovician age for some Highland Border rocks in Central Scotland. J. Geol. Soc. Lond. 139, 451454.CrossRefGoogle Scholar
Donaldson, Colin H. 1983. Tertiary igneous activity in the Inner Hebrides. Proc. Roy. Soc. Edinb. 83B, 6581.Google Scholar
Drury, S. A. 1972. The tectonic evolution of a Lewisian complex on Coll, Inner Hebrides. Scott. J. Geol. 8, 309–33.CrossRefGoogle Scholar
Evans, D., Kenolty, N., Dobson, M. R. and Whittington, R. J. 1980. The geology of the Malin Sea. Rep. lnst. Geol. Sci. 7915.Google Scholar
Evans, D., Chesher, J. A., Deegan, C. E. and Fannin, N. G. T. 1982. The offshore geology of Scotland in relation to the IGS shallow drilling programme, 1970–1978. Rep. lnst. Geol. Sci. 8112.Google Scholar
Gribble, C. D. 1983. Mineral resources. Proc. Roy. Soc. Edinb. 83B, 611625.Google Scholar
Hamilton, P. J., Evensen, N. M., O'nions, R. K. and Tarney, J. 1979. Sm-Nd systematics of Lewisian gneisses. Nature, Lond. 277, 25–8.CrossRefGoogle Scholar
Hickman, A. H. 1975. The stratigraphy of late Precambrian metasediments between Glen Roy and Lismore. Scott. J. Geol. 11, 117–42.CrossRefGoogle Scholar
Jehu, T. J. 1922. The Archaean and Torridonian formations and the later intrusive igneous rocks of Iona. Trans. Roy. Soc. Edinb. 53, 165–87.CrossRefGoogle Scholar
Jelinek, E., Souček, J., Bluck, B. J., Bowes, D.-R. and Treloar, P. J. 1980. Nature and significance of beerbachites in the Ballantrae ophiolites, SW Scotland. Trans. Roy. Soc. Edinb. Earth Sci. 71, 159179.CrossRefGoogle Scholar
Kennedy, W. Q. 1946. The Great Glen fault. Q. Jl Geol. Soc. Lond. 102. 4172.CrossRefGoogle Scholar
Longman, C. D., Bluck, B. J. and van Breemen, O. 1979. Ordovician conglomerates and the evolution of the Midland Valley. Nature, Lond. 280, 578581.CrossRefGoogle Scholar
Lyon, T. D. B. and Bowes, D. R. 1977. Rb-Sr, U:Pb and K-Ar isotopic study of the Lewisian complex between Durness and Loch Laxford, Scotland. Krystalinikum 13, 5372.Google Scholar
Lyon, T. D. B., Pidgeon, R. T., Bowes, D. R. and Hopgood, A. M. 1973. Geochronological investigation of the quartzofeldspathic rocks of the Lewisian of Rona, Inner Hebrides. Q. Jl Geol. Soc. Lond. 129, 389404.CrossRefGoogle Scholar
MacGregor, M. 1965. Excursion guide to the geology of Arran. Geological Society of Glasgow.Google Scholar
McLean, A. C. and Deegan, C. E. 1978. A synthesis of the solid geology of the Firth of Clyde region. In The solid geology of the Clyde sheet (55°N/6°- W), ed. McLean, A. C. and Deegan, C. E. Rep. lnst. Geol. Sci. 78/9, 93–114.Google Scholar
Moorbath, S. Evidence for the age of deposition of the Torridonian sediments of north-west Scotland. Scott. J. Geol. 5, 154–70.CrossRefGoogle Scholar
Peach, B. N.. Horne, J., Gunn, W., Clough, C. T., Hinxman, L. W. and Teall, J. J. M. 1907. The geological structure of the North-West Highlands of Scotland. Mem. Geol. Surv. Scotl.Google Scholar
Peach, B. N., Woodward, H. B., Clough, C. T., Harker, A. and Wedd, C. B. 1910. The geology of Glenelg, Lochalsh and South-east part of Skye. Mem. Geol. Surv. Scotl.Google Scholar
Peacock, J. D. 1983. Quaternary geology of the Inner Hebrides. Proc. Roy. Soc. Edinb. 83B, 8389.Google Scholar
Piasecki, M. A. J. and van Breemen, O. 1979. The ‘Central Highland Granulites’: cover-basement tectonics in the Moine. In The Caledonides of the British Isles-reviewed, ed. Harris, A. L., Holland, C. H. and Leake, B. E. Spec. Publ. Geol. Soc. Lond. 8, 139–144.Google Scholar
Piasecki, M. A. J. and van Breemen, O. 1983. Field and isotopic evidence for a c. 750 Ma tectonothermal event in Moine rocks in the Central Highland region of the Scottish Caledonides. Trans. Roy. Soc. Edinb. Earth Sci. 73, 119134.CrossRefGoogle Scholar
Piasecki, M. A. J. and van Breemen, O. and Wright, A. E. 1981. Late Precambrian of Scotland, England and Wales. In Geology of the North Atlantic Borderlands, ed. Kerr, J. W. and Fergusson, A. J. Mem. Can. Soc. Petrol. Geol. 7, 57–94.Google Scholar
Pringle, J. 1944. The Carboniferous rocks of Glas Eilean, Sound of Islay, Argyllshire. Trans. Geol. Soc. Glasg. 20, 249259.CrossRefGoogle Scholar
Pringle, J. 1952. On the occurrence of Permian rocks in Islay and north Kintyre. Trans. Edinb. Geol. Soc. 14, 297301.CrossRefGoogle Scholar
Rast, N. and Litherland, M. 1970. The correlation of the Ballachulish and Perthshire (Iltay) Dalradian successions. Geol. Mag. 107, 259272.CrossRefGoogle Scholar
Richey, J. E. MacGregor, A. G. and Anderson, F. W. 1961. British Regional Geology. Scotland: The Tertiary Volcanic Districts (3rd edn). Edinburgh: HMSO.Google Scholar
Richey, J. E. Thomas, H. H. 1930. The geology of Ardnamurchan, North-west Mull and Coll. Mem. Geol. Surv. Scotl.Google Scholar
Selley, R. C. 1965. Diagnostic characters of fluviatile sediments of the Torridonian Formation (Precambrian) of northwest Scotland. J. Sedim. Petrol. 35, 366380.CrossRefGoogle Scholar
Simon, J. B. and Bluck, B. J. 1982. Palaeodrainage of the southern margin of the Caledonian mountain chain in the northern British Isles. Trans. Roy. Soc. Edinb. Earth Sci. 73, 1115.CrossRefGoogle Scholar
Smith, D. B., Brunstrom, R. G. W., Manning, P. I., Simpson, S. and Shotton, F. W. 1974. A correlation of Permian rocks in the British Isles. Spec. Rep. Geol. Soc. Lond. 5.Google Scholar
Steiger, R. H. and Jäger, E. 1977. Subcommission on Geochronology: convention on the use of decay constants in geo- and cosmochronology. Earth Planet. Sci. Lett. 36, 359362.CrossRefGoogle Scholar
Stewart, A. D. 1962. On the Torridonian sediments of Colonsay and their relationship to the main outcrop in north-west Scotland. Lpool Manchr Geol. J. 3, 121155.CrossRefGoogle Scholar
Stewart, A. D. 1969. Torridonian rocks of Scotland reviewed. In North Atlantic geology and continental drift—a symposium ed. Kay, M. Mem. Am. Ass. Petrol. Geol. 12, 595–608.Google Scholar
Stewart, A. D. 1975. ‘Torridonian’ rocks of western Scotland. In A correlation of the Precambrian rocks in the British Isles, ed. Harris, A. L. et. al. Spec. Rep. Geol. Soc. Lond. 6, 43–51.Google Scholar
Stewart, A. D. 1982. Late Proterozoic rifting in NW Scotland: the genesis of the ‘Torridonian’. J. Geol. Soc. Lond. 139, 413420.CrossRefGoogle Scholar
Stewart, A. D. Hackman, B. D. 1973. Precambrian sediments of western Islay. Scott. J. Geol. 9, 185201.CrossRefGoogle Scholar
Stewart, A. D. Irving, E. 1975. Palaeomagnetism of Precambrian sedimentary rocks from NW Scotland and the apparent polar wandering path of Laurentia. Geophys. J. Roy. Astr. Soc. 37, 5172.CrossRefGoogle Scholar
Stewart, A. D. Parker, A. 1979. Palaeosalinity and environmental interpretation of red beds from the late Precambrian (‘Torridonian’) of Scotland. Sedim. Geol. 22, 229241.CrossRefGoogle Scholar
Sutton, J. and Watson, J. 1960. Sedimentary structures in the Epidotic Grits of Skye. Geol. Mag. 97, 106–22.CrossRefGoogle Scholar
Sutton, J. and Watson, J. 1964. Some aspects of Torridonian stratigraphy in Skye. Proc. Geol. Ass. 75. 251–87.CrossRefGoogle Scholar
van Breemen, O., Halliday, A. N., Johnson, M. R. W. and Bowes, D. R. 1978. Crustal additions in late Precambrian times. In Crustal evolution in northwestern Britain and adjacent regions, ed. Bowes, D. R. and Leake, B. E. Geol. J. Spec. Issue 10, 81–106.Google Scholar
Westbrook, G. K. 1972. Structure and metamorphism of the Lewisian of east Tiree, Inner Hebrides. Scott. J. Geol. 8, 1330.CrossRefGoogle Scholar
Wilkinson, S. B. 1907. The geology of Islay, including Oronsay and portions of Colonsay and Jura. Mem. Geol. Surv. Scotl.Google Scholar