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Structural Behaviour of Quartzite in a Migmatite Area, Tanganyika

Published online by Cambridge University Press:  01 May 2009

P. E. Brown
P. E. Brown
Affiliation:
Department of Geology, University of Sheffield.
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Abstract

Quartz-magnetite rocks occur as lenses in an area of migmatitic mica gneiss and have acted as resisters to deformation as well as migmatization. Due to plastic deformation in the enclosing gneisses a quartzite lens now strikes perpendicular to the trend of other resisters which are abruptly truncated.

Type
Articles
Information
Geological Magazine , Volume 97 , Issue 3 , June 1960 , pp. 250 - 254
Copyright
Copyright © Cambridge University Press 1960

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References

REFERENCES

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