Abstract
The type locality of the Permian rocks in New South Wales is in the lower Hunter Valley where a complete and continuous sequence occurs. In this area, as well as over most of the Sydney Basin, the Newcastle Coal Measures pass upwards without angular unconformity iuto the overlying Narrabeen Group of Lower Triassic age. The basal glacial shales of the Permian rest also without angular un conformity upon the Kuttung Group of the Carboniferous.
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