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A study was made of the lithology and stratigraphy of an almost complete cored section of uneroded Pandurra Formation. The core was sampled at every change in rock texture and then resampled on the basis of standard textural types.

The aim was to differentiate, using microscopic traits, the McLeay Beds from the Tapley Hill Formation lying above it, and the Pandurra Formation below. The formation boundaries as established by petrography are at variance with the stratigraphic...