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GEOLOGY OF THE - GNS Science

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Figure 11 Steeply dipping beds of centimetre- to metre-bedded Torlesse sandstone and mudstone beside the highway south ofOmaio (Xl51168654) show the fraduring and faulting typical of these rocks. They are unconformably overlain here by Quaternarycolluvial and tephric material. Photo 42148/25: D.L. Homer12

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