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A method for the measurement of volume change

Published online by Cambridge University Press:  01 May 2009

M. Barr  and
M. P. Coward
M. Barr
Affiliation:
Department of Earth SciencesThe UniversityLeeds
M. P. Coward
Affiliation:
Department of Earth SciencesThe UniversityLeeds
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Summary

A method for measuring volume change, which involves combining measurements of the strain ratio with the angle between the surface of no finite longitudinal strain and the principal extension direction in a principal plane, has been used to obtain values for the volume change in two groups of deformed rocks in southern Africa.

Type
Articles
Information
Geological Magazine , Volume 111 , Issue 4 , July 1974 , pp. 293 - 296
Copyright
Copyright © Cambridge University Press 1974

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References

Dunnet, D. 1969. A technique of finite strain analysis using elliptical particles. Tectonophysics 7, 117–36.CrossRefGoogle Scholar
Dunnet, D. & Siddons, A. W. 1971 Non-random sedimentary fabrics and their modification by strain. Tectonophysics 12, 307–25.CrossRefGoogle Scholar
Flinn, D. 1962. On folding during three-dimentional progressive deformation. Q. Jl geol. Soc. Lond. 118, 385–433.CrossRefGoogle Scholar
Huddleston, P. J. 1973. Fold morphology and some geometrical implications of theories of fold development. Tectonophysics 16, 1–46.CrossRefGoogle Scholar
King, R. F. 1966. The magnetic fabric of some Irish granites. Geol. J. 5, 43–66.CrossRefGoogle Scholar
Ramsay, J. G. 1967. Folding and Fracturing of Rocks. McGraw Hill, New York, N.Y. 568 pp.Google Scholar
Ramsay, J. G. & Wood, D. S. 1973. The geometric effects of volume change during deformational processes. Tectonophysics 16, 263–77.CrossRefGoogle Scholar
Ramsey, J. G. & Graham, R. H. 1970. Strain variation in shear belts. Can. J. Earth Sci. 7, 786–813.CrossRefGoogle Scholar
Skempton, A. W. 1970. The consolidation of clays by gravitational compaction. Q. Jl. geol. Soc. Lond. 125, 373–411.CrossRefGoogle Scholar
Sorby, H. C. 1853. On the origin of slaty cleavage. Edin. New Philos. J. 55, 137–48.Google Scholar
Sorby, H. C. 1908. On the application of quantitative methods to the study of rocks. Q. Jl. geol. Soc. Lond. 64, 171–232.CrossRefGoogle Scholar
Talbot, C. J. 1970. The minimum strain ellipsoid using deformed quartz veins. Tectonophysics 9, 47–76.CrossRefGoogle Scholar