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Wall-rock silicification associated with fluorite veins in Carboniferous limestone at Butts Quarry, Derbyshire, England

Published online by Cambridge University Press:  01 May 2009

R. Kanaris-Sotiriou ,
R. Neves  and
F. G. F. Gibb
R. Kanaris-Sotiriou
Affiliation:
Department of Geology, University of Sheffield, S1 3JD, UK
R. Neves
Affiliation:
Department of Geology, University of Sheffield, S1 3JD, UK
F. G. F. Gibb
Affiliation:
Department of Geology, University of Sheffield, S1 3JD, UK
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Abstract

Wall rocks on either side of narrow fluorite veins cutting Dinantian Limestones at Butts Quarry, Derbyshire, exhibit unusual and spectacular alteration structures. Buff, ‘blackened’ and grey limestone lithologies, containing significant amounts of euhedral quartz crystals, occur in a zoned sequence adjacent to the veins. The alteration structures are attributed to a two-stage process involving silicification and subsequent re-mobilization of silica by fluids passing along the vein.

Type
Articles
Information
Geological Magazine , Volume 123 , Issue 5 , September 1986 , pp. 569 - 579
Copyright
Copyright © Cambridge University Press 1986

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References

Aitkenhead, N. & Chisholm, J. I. 1982. A standard nomenclature for the Dinantian formations of the Peak District of Derbyshire and Staffordshire. Institute of Geological Sciences Report No. 82/8, London: HMSO, 17 pp.Google Scholar
Arnold-Bemrose, H. H. 1898. On a quartz-rock in the Carboniferous Limestone of Derbyshire. Quarterly Journal of the Geological Society of London 54, 169–83.Google Scholar
Ford, T. D. 1976. The ores of the south Pennines and Mendip Hills, England – a comparative study. In Handbook of Strata-bound and Stratiform Ore Deposits, Volume 5: Regional Studies (ed. Wolf, K. H.), pp. 161–95. Amsterdam: Elsevier.Google Scholar
Fyfe, W. S., Price, N. J. & Thompson, A. B. 1978. Fluids in the Earth's Crust (Developments in Geochemistry; 1). Amsterdam: Elsevier, 383 pp.Google Scholar
George, T. N., Johnson, G. A. L., Mitchell, M., Prentice, J. E., Ramsbottom, W. H. C., Sevastopulo, G. D. & Wilson, R. B. 1976. A correlation of Dinantian rocks in the British Isles. Geological Society of London Special Report, No. 7.Google Scholar
Harrison, D. J. & Adlam, K. A. MCL. 1985. Limestones of the Peak. British Geological Survey Mineral Assessment Report 144. London: HMSO.Google Scholar
Ineson, P. R. 1970. Trace-element aureoles in limestone wallrocks adjacent to fissure veins in the Eyam area of the Derbyshire ore field. Transactions of the Institution of Mining and Metallurgy (Section B) 79, B238–B245.Google Scholar
Ineson, P. R. & Ford, T. D. 1982. The south Pennine orefield: its genetic theories and eastward extension. Mercian Geologist 8 (4), 285–303.Google Scholar
Kelman, P. M. 1980. The Lower Carboniferous volcanic rocks of the Ashover area, Derbyshire. Mercian Geologist 8, 11–28.Google Scholar
Orme, G. R. 1974. Silica in the Visean limestones of Derbyshire, England. Proceedings of the Yorkshire Geological Society 40 (5), 63–104.CrossRefGoogle Scholar
Rhys, G. H. 1967. The Ashover Area. In Geological excursions in the Sheffield region and the Peak District National Park (eds. Neves, R. Downie, C.). University of Sheffield.Google Scholar
Rogers, P. J. 1977. Fluid inclusion studies in fluorite from the Derbyshire orefield. Transactions of the Institution of Mining and Metallurgy (Section B) 88, B128–132.Google Scholar
Smith, E. G., Rhys, G. H. & Eden, R. A. 1967. Geology of the country around Chesterfield, Matlock and Mansfield. Memoir of the Geological Survey of Great Britain. London: HMSO.Google Scholar
Sweeting, G. S. 1946. An outline of the geology of Ashover, Derbyshire. Proceedings of the Geologists Association 57, 117–36.Google Scholar