Abstract
The continental mass of Australia (Fig. 8.1) is made up of four great structural units, to which we may add a fifth represented in the fringing island arcs to the north and east. The oldest and most extensive unit is the Precambrian craton which comprises most of the central and western parts of the continent where Precambrian rocks are exposed beneath an intermittent Phanerozoic cover.
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© 1975 The Estate of the late H. H. Read and Janet Watson
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Read, H.H., Watson, J. (1975). The Australian Craton. In: Introduction to Geology. Palgrave, London. https://doi.org/10.1007/978-1-349-15609-2_8
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DOI: https://doi.org/10.1007/978-1-349-15609-2_8
Publisher Name: Palgrave, London
Print ISBN: 978-0-333-17667-2
Online ISBN: 978-1-349-15609-2
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