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Strain and shape analysis from the deformed pyrites with a note on their preferred orientation

Published online by Cambridge University Press:  01 May 2009

R. Sen
Affiliation:
Belikvassli Gruber A/S, North Norway
A. D. Mukherjee
Affiliation:
Institütt for GeologyUniversitet i Oslo, Norway

Summary

From the distribution and orientation of final axial ratios of deformed elliptical pyrites and boudins, initial distributions are determined. A strain ellipse is then reconstructed using the shape factor grid. The long axis of the strain ellipsoid represents the trend of regional fold axis (the fold is of flexural slip type). The dimensional orientation (elongation) of the pyrites and the boudins is referred to the homogeneous strain components in the fold. Petrofabrics of the pyrite cubes indicate that they have a preferred orientation.

Type
Articles
Copyright
Copyright © Cambridge University Press 1972

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References

Cloos, E. 1947. Oölite deformation in the South Mountain Fold, Maryland. Bull. geol. Soc. Am. 58, 843918.CrossRefGoogle Scholar
Dunnet, D. 1969. A technique of finite strain analysis using elliptical particles. Tectono-physics 7, 117–36.CrossRefGoogle Scholar
Elliot, D. 1968. Determination of Finite Strain and Initial Shape from deformed elliptical objects. Spec. Pap. geol. Soc. Am. 115, 57 p.Google Scholar
Elliot, D. 1970. Determination of finite strain initial shape from deformed elliptical objects. Bull. geol. Soc. Am. 81, 2221–36.CrossRefGoogle Scholar
Flinn, D. 1956. On the deformation of Funzie conglomerate, Fetlar, Shetland. J. Geol. 64, 480505.CrossRefGoogle Scholar
Gay, N. C. 1969. The analysis of strain in the Barbuton Mountain Land, eastern Transvaal, using deformed pebbles. J. Geol. 77, 377–96.CrossRefGoogle Scholar
Griffiths, J. C. 1967. Scientific method in analysis of sediments. 508 pp. McGraw Hill, New York.Google Scholar
Hossack, J. R. 1968. Pebble deformation and thrusting in the Bygolin area (southern Norway). Tectonophysics 5, 315–39.CrossRefGoogle Scholar
Ramberg, H. & Ekström, T. 1964. Note on preferred orientation of pyrite cubes in grit layers in slate. Neues Jb. Miner. Mh. Jan, 246–51.Google Scholar
Ramberg, I. B. 1967. Kongsfjell–Områdets geologi, en petrografisk og strukturall undersøkelse i helgeland, Nord-Norge (in Norwegian). Norg. geol. unders. 240, 152.Google Scholar
Ramsay, J. G. 1967. Folding and fracturing of rocks. 568 pp. McGraw Hill, New York.Google Scholar
Vokes, F. M. 1963. Geological studies on the Caledonian pyritic zinc–lead ore body at Bleikvassli, Nordland, Norway. Norg. geol. unders. 222, 1126.Google Scholar