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Magnetic Grain Fabric Studies of the Middle Coal Measures of the Southern Part of the South Staffordshire Coalfield

Published online by Cambridge University Press:  01 May 2009

H. ab Iorwerth ,
N. Hamilton  and
P. J. Loveland
H. ab Iorwerth
Affiliation:
Department of Geology, The University, Southampton.
N. Hamilton
Affiliation:
Geophysics Section, Department of Geology, University of Birmingham, P.O. Box 363, Birmingham 15.
P. J. Loveland
Affiliation:
Geophysics Section, Department of Geology, University of Birmingham, P.O. Box 363, Birmingham 15.
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Abstract

Measurement of the anisotropy of magnetic susceptibility of Westphalian sandstones from the southern part of the South Staffordshire Coalfield shows that there is a weak preferred grain orientation. There is a significant within-sample consistency of fabric lineation and the results agree with other geological evidence. The palaeocurrent pattern is complex as may be expected within a fluvial or deltaic regime. This preliminary study suggests that this magnetic fabric technique may be used to determine the detailed palaeocurrent pattern within the Upper Carboniferous of the Midland Province.

Type
Articles
Information
Geological Magazine , Volume 104 , Issue 6 , December 1967 , pp. 564 - 573
Copyright
Copyright © Cambridge University Press 1967

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References

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