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A survey of white mica crystallinity and polytypes in pelitic rocks of Snowdonia and Llŷn, North Wales

Published online by Cambridge University Press:  05 July 2018

R. J. Merriman
Affiliation:
British Geological Survey, Keyworth, Nottingham NG12 5GG
B. Roberts
Affiliation:
Department of Geology, Birkbeck College, University of London, 7-15 Gresse Street, London W1P 1PA

Abstract

Pelitic rocks in North Wales, ranging in age from late Precambrian to Silurian were sampled. XRD analysis was used to determine the mineralogy and white mica crystallinity of separated < 2 µm fractions. Results show that three stages of metapelite recrystallization can be distinguished. Stage I metapelites are uncleaved or feebly cleaved with crystallinities > 0.43Δ°2θ; the 1Md polytype dominates < 2 µm fractions, occurring as K-and Na-micas. Stage II metapelites show variable cleavage development and crystallinities in the range 0.26-0.43Δ°2θ; 1Md and 2M1 polytypes occur and K- and Na-micas are commonly regularly interstratified. Stage III metapelites are strongly cleaved with crystallinities < 0.26Δ°2θ; the 2M1 polytype is dominant, occurring as K-mica and paragonite. Pelites bearing pyrophyllite, rectorite, and corrensite are found close to plug-like intrusions and were contact altered prior to regional metamorphism. 1M mica is common in deeply buried but relatively undeformed volcaniclastic rocks of the Arfon Group.

Contours of equal crystallinity (isocrysts) are plotted with metabasite zones on a metamorphic map. This shows that stage I metapelites are equivalent to the subpumpellyite zone (≡?laumontite zone). Stage II metapelites are equivalent to the prehnite-pumpellyite facies and stage III metapelites to the clinozoisite and biotite zones of the greenschist facies.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1985

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References

Bailey, S. W. (1980) In Crystal Structures of Clay Minerals and their Identification (Brindley, G. W. and Brown, G., eds.). Mineralogical Society, London, 1123.Google Scholar
Brindley, G. W. (1980) Ibid. 125-95.Google Scholar
British Geological Survey (1985) 1:50000 Sheet 106, Bangor.Google Scholar
Coward, M. P., and Siddans, A. W. B. (1979) In The Caledonides of the British Isles—reviewed (Harris, A. L., Holland, C. H., and Leake, B. E., eds.). Geol. Soc. London Special Publication No. 8, 187-98.CrossRefGoogle Scholar
Croudace, I. W. (1982) Geochim. Cosmochim. Acta, 46, 609-22.CrossRefGoogle Scholar
Eslinger, E. V., and Savin, S. M. (1973) Am. J. Sci. 273, 240-67.CrossRefGoogle Scholar
Frey, M. (1969) Contrib. Mineral. Petrol. 24, 63-5.CrossRefGoogle Scholar
Gill, W. D., Khalaf, F. I., and Massoud, M. S. (1977) Sedimentology, 24, 675-94.CrossRefGoogle Scholar
Kisch, H. J. (1966) Am. J. Sci. 264, 386-97.CrossRefGoogle Scholar
Kisch, H. J. (1980) J. geol. Soc. London, 137, 27188.CrossRefGoogle Scholar
Kisch, H. J. (1983) In Developments in Sedimentology 25B. (Larsen, G. and Chilingar, G. V., eds.). Elsevier, 289493.Google Scholar
Knipe, R. J. (1981) Tectonophysics, 78, 249-72.CrossRefGoogle Scholar
Kossovskaya, A. G., and Shutov, V. D. (1965) Intern. Geol. Rev. 7, 1157-67.CrossRefGoogle Scholar
Kubler, B. (1967) In “Etages tectonique’, Colloque à Neuchâtel, Institut de Geologic de l'Université de Neuchâttel, 105-22.Google Scholar
Kubler, B. (1968) Bull. Centre Rech. Pau-SNPA, 2, 385-97.Google Scholar
Matley, C. A. (1928) Q. J. Geol. Soc. Lond. 84, 440504.CrossRefGoogle Scholar
Nadeau, P. H., Tait, J. M., McHardy, W. J., and Wilson, M. J. (1984) Clay Minerals, 19, 6776.Google Scholar
Nadeau, P. H., Wilson, M. J., McHardy, W. J., and Tait, J. M. (1985) Mineral. Mag. 49, 393-400.CrossRefGoogle Scholar
Reedman, A. J., Leveridge, B. E., and Evans, R. B. (1984) Proc. Geol. Ass. 95, 313-21.CrossRefGoogle Scholar
Roberts, B. (1979) The Geology of Snowdonia and Llýn. Adam Hilger, Bristol.Google Scholar
Roberts, B. (1981) Geol. Mag. 118, 189-200.CrossRefGoogle Scholar
Sudo, T., Hayashi, H., and Shimoda, S. (1962) In Clays and Clay Minerals, Proc. Natl. Conf. Clay Mineral. 9th, 1960. 378-92.Google Scholar
Triplehorn, D. M. (1967) J. Sediment. Petrol. 37, 879-84.CrossRefGoogle Scholar
Velde, B. (1965) Am. Mineral. 50, 436-49.Google Scholar
Velde, B. (1969) Bull. Soc. Fr. Mineral. Cristallogr. 92, 360-8.Google Scholar
Wood, D. S. (1969) In The Pre-Cambrian and Lower Palaeozoic Rocks of Wales (Wood, A., ed.). Univ. Wales, Cardiff, 4766.Google Scholar