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Geochronological evidence for phased volcanic activity in Fife and Caithness necks, Scotland

Published online by Cambridge University Press:  03 November 2011

R. M. Macintyre
Affiliation:
Isotope Geology Unit, Scottish Universities Research and Reactor Centre, East Kilbride, Glasgow G75 0QU, Scotland
R. A. Cliff
Affiliation:
Department of Earth Sciences, University of Leeds, Leeds LS2 9JT, England
N. A. Chapman
Affiliation:
Environmental Protection Unit, Institute of Geological Sciences, Building 151, Harwell Laboratory, Didcot, Oxon OX11 ORA, England

Abstract

In an attempt to establish a chronology for volcanic neck emplacement and so elucidate petrogenesis, isotopic studies have been carried out on various cumulate inclusions, blocks and megacrysts which occur chiefly in association with tuffs infilling several Scottish vents. K-Ar ages of 13 samples of low-pressure cumulate minerals (biotite, hornblende and pyroxene) from necks in East Fife indicate crystallisation at shallow depth at 314 Ma. U-Pb analyses of zircons are concordant at 318 Ma suggesting they are also members of this suite and their formation is penecontemporaneous with the Namurian volcanic activity which is welldocumented stratigraphically. By 295 Ma crystallisation of anorthoclase megacrysts had been completed, perhaps from the fractionated residuum. An eruption from considerable depth (within the stability field of garnet precipitation) then broke through to the surface bearing high-pressure megacrysts. This penetrated and disrupted the early cumulates carrying them to the surface and producing the diverse vent assemblages. K-Ar dating of basanites suggest that the Duncansby Ness neck in Caithness was emplaced around 270 Ma in the early Permian. For two Fife necks the balance of evidence favours an age of 290 Ma (Stephanian) for this final explosive activity associated with vent formation.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1981

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References

Balsillie, D. 1920. Descriptions of some new volcanic vents in East Fife. Trans Edinburgh Geol Soc 11, 81–5.CrossRefGoogle Scholar
Balsillie, D. 1923. Further observations on the volcanic geology of East Fife. Geol Mag 60, 530–42.CrossRefGoogle Scholar
Balsillie, D. 1927. Contemporaneous volcanic activity in East Fife. Geol Mag 64, 481–94.CrossRefGoogle Scholar
Boulton, W. S. 1911. On a monchiquite intrusion in the Old Red Sandstone of Monmouthshire. Q J Geol Soc London 67, 460–75.CrossRefGoogle Scholar
Chapman, N. A. 1974. Petrology of inclusions from late Palaeozoic British volcanic rocks. Unpublished Ph.D thesis, University of Edinburgh.Google Scholar
Chapman, N. A. 1975. An experimental study of spinelclinopyroxenite xenoliths from the Duncansby Ness vent, Caithness, Scotland. Contrib Mineral Petrol 51, 223–30.CrossRefGoogle Scholar
Chapman, N. A. 1976. Inclusions and megacrysts from undersaturated tuffs and basanites, East Fife, Scotland. J Petrol 17, 472–98.CrossRefGoogle Scholar
Chapman, N. A. & Powell, R. 1976. Origin of anorthoclase megacrysts in alkali basalts. CONTRIB MINERAL PETROL 58, 2935.CrossRefGoogle Scholar
Coe, K. 1966. Intrusive tuffs of west Cork, Ireland. Q J GEOL SOC LONDON 122, 128.CrossRefGoogle Scholar
Colvine, R. J. L. 1968. Pyrope from Elie, Fife. SCOTT J GEOL 4, 283–6.CrossRefGoogle Scholar
dimming, G. A. 1936. The structural and volcanic geology of the Elie-St. Monance district. TRANS EDINBURGH GEOL SOC 13, 340–65.Google Scholar
de Souza, H. A. F. 1979. he geochronology of Scottish Carboniferous volcanism. Unpublished Ph.D. thesis, University of Edinburgh.Google Scholar
Donaldson, C. H. 1978. Petrology of the uppermost upper mantle deduced from spinel-lherzolite and harzburgite nodules at Calton Hill, Derbyshire. CONTRIB MINERAL PETROL 65, 363–77.CrossRefGoogle Scholar
Fitch, F. J., Miller, J. A. & Williams, S. C. 1970. Isotopic ages of British Carboniferous rocks. C R 6e CONGR INT STRATIGR GEOL CARBONIFEROUS 2, 771–90.Google Scholar
Forsyth, I. H. & Rundle, C. C. 1978. The age of the volcanic and hypabyssal rocks of East Fife. BULL GEOL SURV G.B. 60, 23–9.Google Scholar
Francis, E. H. 1977. Volcanic necks, In Forsyth, I. H. & Chisholm, J. I. The Geology of East Fife, 171220. MEM GEOL SURV G.B.Google Scholar
Francis, E. H. & Hopgood, A. M. 1970. Volcanism and the Ardross Fault, Fife. SCOTT J GEOL 6, 162–85.CrossRefGoogle Scholar
Geikie, A. 1879. On the Carboniferous volcanic rocks of the basin of the Firth of Forth – their structure in the field and under the microscope. TRANS R SOC EDINBURGH 29, 437518.CrossRefGoogle Scholar
Hamad, S. El D. 1963. The chemistry and mineralogy of olivine nodules from Calton Hill, Derbyshire. MINERAL MAG 33, 483–97.Google Scholar
Krogh, T. E. 1973. A low contamination method for hydrothermal decomposition of zircon and extraction of U and Pb for isotopic age determination. GEOCHIM COSMOCHIM ACTA 37, 485–94.CrossRefGoogle Scholar
Krogh, T. E. & Davis, G. L. 1974. Alteration of zircons with disordant U-Pb ages. CARNEGIE INST WASHINGTON YEARB 73, 560–7.Google Scholar
Macdonald, R., Thomas, J. E. & Rizzello, S. A. 1977. Variations in basalt chemistry with time in the Midland Valley province during the Carboniferous and Permian. SCOTT J GEOL 13, 1122.CrossRefGoogle Scholar
McDougall, I., Maier, R., Sutherland-Hawkes, P. & Gleadow, A. J. W. 1980. K-Ar age estimate for the KBS tuff, East Turkana, Kenya. NATURE LONDON 284, 230–4.CrossRefGoogle Scholar
Macintyre, R. M., Mitchell, J. G. & Dawson, J. B. 1974. Age of fault movements in Tanzanian sector of the East African Rift System. NATURE LONDON 247, 354–6.CrossRefGoogle Scholar
Macintyre, R. M., York, D. & Moorhouse, W. M. 1967. Potassiumargon age determinations in the Madoc-Bancroft area in the Grenville Province of the Canadian Shield. CAN J EARTH SCI 4, 815–28.CrossRefGoogle Scholar
Purdy, J. W. & Jager, E. 1976. K-Ar ages on rock-forming minerals from the Central Alps. MEM 1ST GEOL MINERAL UNIV PADOVA 30, 31 pp.Google Scholar
Steiger, R. H. & Jäger, E. 1977. Subcommission on geochronology: convention on the use of decay constants in geo- and cosmochronology. EARTH PLANET SCI LETT 36, 359–62.CrossRefGoogle Scholar
Tera, F. & Wasserburg, G. J. 1972. U-Th-Pb systematics in three Apollo 14 basalts and the problem of initial lead in lunar rocks. EARTH PLANET SCI LETT 14, 281304.CrossRefGoogle Scholar
Walker, G. P. L. & Ross, J. V. 1954. A xenolithic monchiquitic dyke near Glenfinnan, Inverness-shire. GEOL MAG 91, 463–72.CrossRefGoogle Scholar
Whyte, F. 1963. The Heads of Ayr vent. TRANS GEOL SOC GLASGOW 25, 7297.CrossRefGoogle Scholar