1887
Volume 3, Issue 2
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

Detailed and reconnaissance airborne magnetic data over a 150 square mile tract in the Parkes area N.S.W. have been compared and used to investigate the magnetic response and distribution of Ordovician vol-canics and metasediments which occur in the area.

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/content/journals/10.1071/EG972201
1972-06-01
2026-01-17
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References

  1. ANDREWS, E.C. 1910. The Forbes-Parkes Goldfield. Min. Res. 13 Dept. Mines N.S.W. 109 pp.
  2. CARTER, R.M. 1960. Forbes-West Wyalong and Bourke areas, Airborne Magnetic and Radiometric Survey N.S.W. 1960. Rec. 1960/105. Bur. Min. Res. Geol. & Geophys. 8 pp.
  3. FACER, R.A. 1968. Some results of a reconnaissance magnetic investigation of Ordovician rocks from central western New South Wales. Aust. J. Sci. 31/3 pp.120-121.
  4. PACKHAM, G.H. (Ed.) 1969. The Geology of New South Wales. Jour. Geol. Soc. Aust. Vol. 16 part 1 65 pp.
  5. SHERWIN, L. 1972. New stratigraphic units from the Forbes district. Quart. Notes N.S.W. Geol. Survey No. 6, pp. 1-2.
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  • Article Type: Research Article

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