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Genesis of the graphite deposit at Seathwaite in Borrowdale, Cumbria

Published online by Cambridge University Press:  01 May 2009

J. Parnell
J. Parnell
Affiliation:
Department of Geology, Imperial College of Science and Technology, London S.W.7
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Abstract

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Type
Correspondence
Information
Geological Magazine , Volume 119 , Issue 5 , September 1982 , pp. 511 - 512
Copyright
Copyright © Cambridge University Press 1982

References

Breger, I. A. 1963. Origin and classification of naturally occurring carbonaceous substances. Int. Ser. Mon. Earth Sciences 16, 50–86.Google Scholar
Brown, G. C., Cassidy, V., Oxburgh, E. R., Plant, J., Sabine, P. A. & Watson, J. V. 1980. Basement heat flow and metalliferous mineralization in England and Wales. Nature 288, 657–9.CrossRefGoogle Scholar
Glassley, W. 1982. Fluid evolution and graphite genesis in the deep continental crust. Nature 295, 229–31.CrossRefGoogle Scholar
Jacob, H. 1967. Petrologie von asphaltiten und asphaltische pyrobitumina. Erdol und Kohle 20, 393–400.Google Scholar
King, L. H., Goodspeed, F. E. & Montgomery, D. S. 1963. A study of sedimented organic matter and its natural derivatives. Rep. Dep. Mines tech. Survs Can. 114.Google Scholar
Marmo, V. 1953. Schungite – a precambrian carbon. Geol. Foren. Stockh. 75, 89–96.CrossRefGoogle Scholar
Marr, J. E. 1916. The geology of the Lake District and the scenery as influenced by geological structure. Cambridge: Cambridge University Press.Google Scholar
Mitchell, J. G. & Ineson, P. R. 1975. Potassium-argon ages from the graphite deposits and related rocks of Seathwaite, Cumbria. Proc. Yorks. geol. Soc. 40, 413–18.CrossRefGoogle Scholar
Mueller, G. 1960. The distribution of uranium in naturally fractionated organic phases. (Abs.) Rpt 21st Int. Geol. Congress (Norden), 143.Google Scholar
Nalivkin, D. V. 1973. Geology of the U.S.S.R. (English translation). Toronto: University of Toronto Press.Google Scholar
Osborne, C. B. 1923. A theory to account for occurrence of oil in the vesicular cavities of igneous intrusions. Bull. Am. Ass. Petrol. Geol. 7, 288–90.Google Scholar
Rankama, K. 1948. New evidence of the origin of precambrian carbon. Bull. Geol. Soc. Am. 59, 389–416.CrossRefGoogle Scholar
Rundle, C. C. 1979. Ordovician intrusions in the English Lake District. J. geol. Soc. 136, 29–38.CrossRefGoogle Scholar
Strens, R. G. T. 1965. The graphite deposit of Seathwaite in Borrowdale, Cumberland. Geol. Mag. 102, 393–406.CrossRefGoogle Scholar
Sudovikov, N. G. 1937. Geological sketch of the Zaonezhye Peninsula. In Northern Excursion Guide, 17th Int. Geol. Congress (Moscow), 45–58.Google Scholar
Weis, P. L., Friedman, I. & Gleason, J. P. 1981. The origin of epigenetic graphite: evidence from isotopes. Geochim. cosmochim. Acta 45, 2325–32.CrossRefGoogle Scholar