Abstract
Large biotite grains, up to 1 metre across, in a pegmatite near Broken Hill, Australia, have been heterogeneously deformed and partly recrystallized in zones of relatively high strain, probably under conditions of the lower amphibolite facies. Many of the new aggregates (which consist mainly of more magnesian biotite, with muscovite, and less abundant ilmenite and albite) have a mica preferred orientation. Some of the oriented mica aggregates have grown in kink-like deformation zones (some of which appear to have involved fracturing) and others have grown in dilatation zones (growth of mica probably keeping pace with the opening of the zones). The shapes and preferred orientation of new mica grains appear to be due to varying contributions by (a) mechanical rotation of slices cleaved parallel to (001), (b) coaxial nucleation and/or growth of new mica on rotated portions of deformed biotite, and (c) preferred nucleation and/or growth of new grains in directions of minimum mechanical constraint and maximum transport of chemical components. This preferred growth can also explain the observed high degree of elongation of the oriented mica grains.
Similar content being viewed by others
References
Binns, R.A.: Zones of progressive regional metamorphism in the Willyama Complex, Broken Hill district, New South Wales. J. Geol. Soc. Australia 11, 283–330 (1964)
Etheridge, M.A.: Experimental investigations of the mechanisms of mica preferred orientation in foliated rocks. Unpub. Ph.D. thesis, Australian National University, Canberra (1971)
Etheridge, M.A.: Crystallization and recrystallization of layer silicates during deformation. Unpublished abstract, University of Leiden Microstructure Conference (1976)
Etheridge, M.A., Hobbs, B.E.: Chemical and deformational controls on recrystallization of mica. Contrib. Mineral. Petrol. 43, 111–124 (1974)
Etheridge, M.A., Hobbs, B.E., Paterson, M.S.: Experimental deformation of single crystals of biotite. Contrib. Mineral. Petrol. 38, 21–36 (1973)
Phillips, N., Lee, S.D., Wall, V.J.: Metamorphism and mineralisation in the Broken Hill district, N.S.W. 25th International Geological Congress, Abstracts, 1, 136–137 (1976)
Ramsay, J.G.: Development of chevron folds. Bull. Geol. Soc. Am. 85, 1741–1754 (1974)
Vernon, R.H.: Microstructures of high-grade metamorphic rocks at Broken Hill, Australia. J. Petrol. 9, 1–22 (1968)
Vernon, R.H.: The Willyama Complex, Broken Hill area. J. Geol. Soc. Australia 16, 20–56 (1969)
Vernon, R.H., Ransom, D.M.: Retrograde schists of the amphibolite facies at Broken Hill, New South Wales. J.Geol. Soc. Australia 18, 267–277 (1971)
Weiss, L.E.: The minor structures of deformed rocks. Berlin-Heidelberg-New York: Springer 1972
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Vernon, R.H. Microfabric of mica aggregates in partly recrystallized biotite. Contrib. Mineral. Petrol. 61, 175–185 (1977). https://doi.org/10.1007/BF00374366
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/BF00374366