Hostname: page-component-586b7cd67f-g8jcs Total loading time: 0 Render date: 2024-11-26T01:09:19.125Z Has data issue: false hasContentIssue false
  • English
  • Français

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.
Get access Rights & Permissions [Opens in a new window]

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

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Crimes, T. P., and Oldershaw, M. A., 1967. Palaeocurrent determinations by magnetic fabric measurements on the Cambrian rocks of St. Tudwal's Peninsula, North Wales. Geol. J., 5, 217–232.CrossRefGoogle Scholar
Curray, J. R., 1956. The analysis of two-dimensional orientation data. J. Geol, 64, 117–131.CrossRefGoogle Scholar
Graham, J. W., 1967. The significance of magnetic anisotropy in Appalachian sedimentary rocks. (In Steinhart, J., and Smith, J., Edit., Am. geophys. Union, Monogr. No. 10.)Google Scholar
Granar, L., 1958. Magnetic measurements on Swedish varved sediments. Arkiv. Geofysik, 3, 1–40.Google Scholar
Hamilton, N., 1963. Susceptibility anisotropy measurements on some Silurian siltstones. Nature, Lond., 197, 170–1.CrossRefGoogle Scholar
Hamilton, N., and Loveland, P. J., 1967. Some preliminary susceptibility anisotropy measurements on greywackes from the Trinity Peninsula Series of Graham Land. Bull. Br. Antarct. Surv., 11, 59–71.Google Scholar
Hamilton, N., and Rees, A. I., in preparation. The anisotropy of magnetic susceptibility of the Franciscan rocks of the Diablo Range, Central California.Google Scholar
Hamilton, N., Owens, W. H., and Rees, A. I., in preparation. Laboratory experiments on the production of grain orientation in shearing sand.Google Scholar
Jukes, J. B., 1859. The South Staffordshire Coalfield. Mem. Geol. Surv. U.K.Google Scholar
King, R. F., and Rees, A. I., 1962. The measurement of the anisotropy of magnetic susceptibility of rocks by the torque method. J. geophys. Res., 67, 1565–1572.CrossRefGoogle Scholar
Rees, A. I., 1961. The effect of water currents on the magnetic remanence and anisotropy of susceptibility of some sediments. Geophys. J., 5, 235–251.CrossRefGoogle Scholar
Rees, A. I., 1964. Measurements of the Natural Remanent Magnetism and Anisotropy of Susceptibility of some Swedish Glacial Silts. Geophys. J., 8, 356–369.CrossRefGoogle Scholar
Rees, A. I., 1965. The use of anisotropy of magnetic susceptibility in the estimation of sedimentary fabric. Sedimentology, 4, 257–271.CrossRefGoogle Scholar
Rees, A. I., 1966. The effect of depositional slopes on the anisotropy of magnetic susceptibility of laboratory deposited sands. J. Geol., 74, 856–867.CrossRefGoogle Scholar
Trueman, A. E., 1940. The lamellibranch zones of the South Staffordshire Coalfield. Geol. Mag., 77, 28–41.CrossRefGoogle Scholar
von Rad, U., and Rees, A. I., in preparation. Magnetic Fabric of sediments from the La Jolla Submarine Canyon and Fan (California).Google Scholar
Wills, L. J., 1935. An outline of the palaeogeography of the Birmingham country. Proc. Geol. Ass., 66, 1–36.Google Scholar
Wills, L. J., 1948. Palaeogeography of the Midlands, University Press of Liverpool. 147 pp.Google Scholar
Wills, L. J., 1956. Concealed Coalfields, Blackie, London, 208 pp.Google Scholar