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A Magnetic Fabric in Till

Published online by Cambridge University Press:  01 May 2009

M. D. Fuller
M. D. Fuller
Affiliation:
Scripps Institute of Oceanography, La Jolla, California.
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Abstract

The magnetic susceptibility anisotropy of specimens of a glacial till is described and used to define a magnetic fabric. This is compared with the fabric established by small particle and stone orientation. The maximum susceptibility direction is shown to be similar to the preferred direction of the long axes of particles and stones.

Type
Articles
Information
Geological Magazine , Volume 99 , Issue 3 , June 1962 , pp. 233 - 237
Copyright
Copyright © Cambridge University Press 1962

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References

REFERENCES

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