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Proterozoic Palaeocurrent directions in the Kimberley Region, Northwestern Australia

Published online by Cambridge University Press:  01 May 2009

D. C. Gellatly
Affiliation:
Bureau of Mineral Resources, Geology, and Geophysics, P.O. Box 378, Canberra City, 2601, Australia
G. M. Derrick
Affiliation:
Bureau of Mineral Resources, Geology, and Geophysics, P.O. Box 378, Canberra City, 2601, Australia
K. A. Plumb
Affiliation:
Bureau of Mineral Resources, Geology, and Geophysics, P.O. Box 378, Canberra City, 2601, Australia

Summary

Palaeocurrent directions from cross-beds in the Proterozoic Kimberley Basin sediments, north-western Australia indicate sediment transport predominantly from the north-east in the lower part of the succession, and from the north-west in the middle and upper parts. Most of the sediment was probably derived from the north and only a little from the adjacent exposed areas of older Pre-Cambrian rocks to the south. The suggested northerly source of the sediment is consistent with a probable former position of Western Australia close to Peninsular India and to Burma.

Type
Articles
Copyright
Copyright © Cambridge University Press 1970

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References

REFERENCES

Allen, J. R. L. 1963. Classification of cross stratified units with notes on their origin. Sedimentology, 2 (2), 93114.CrossRefGoogle Scholar
Bofinger, V. M. 1967. Geochronology of the East Kimberley region, Western Australia. Aust. N.Z. Ass. Advmt Sci., Abst.. Vol. 110–111.Google Scholar
Carey, S. W. 1958. A tectonic approach to continental drift. Symposium on Continental Drift: Univ. of Tasmania, p. 177.Google Scholar
Crawford, A. R. (In press). India, Australia, and Indian continental re-assembly. Nature, Lond.Google Scholar
Creer, K. M. 1965. Palaeomagnetic data from the Gondwanic continents. Phil. Trans. R. Soc. Lond. Ser. A, 258(1088), 2740.Google Scholar
Dunn, P. R., Plumb, K.A., & Roberts, H. G. 1966. A proposal for time-stratigraphic subdivision of the Australian Precambrian. J. geol. Soc. Aust. 13(2), 593608.CrossRefGoogle Scholar
Gellatly, D. C., & Derrick, G. M. 1969. Lansdowne, Western Australia 1:250,000 Geological Series. Bur. miner. Resour. Aust., explan. Notes SE/52–5.Google Scholar
Gellatly, D. C., Sofoulis, J., & Derrick, G. M. (In press). The Precambrian Geology of the Kimberley Region: The West Kimberley. Bull. Bur. miner. Resour. Aust.Google Scholar
McDougall, I., Dunn, P. R., Compston, W., Webb, A. W., Richards, J. R., & Bofinger, V. M. 1965. Isotopic age determinations on Precambrian rocks of the Carpentaria Region, Northern Territory, Australia. J. geol. Soc. Aust., 12(1), 6790.CrossRefGoogle Scholar
McKee, E. D., & Weir, G. W. 1953 Terminology for stratification and cross-stratification in sedimentary rocks. Bull. geol. Soc. Am., 64, 381390.CrossRefGoogle Scholar
Plumb, K. A. (In press). The Precambrian Geology of the Kimberley Region: The Kimberley Basin. Bull. Bur. miner. Resour. Aust.Google Scholar
Stride, A. H. 1963. Current-swept sea floors near the southern half of Great Britain. Q. Jl geol. Soc., Lond. 119, 175200.CrossRefGoogle Scholar
Wegener, A. 1924. The Origins of Continents and Oceans. Methuen & Co., London.Google Scholar