Marla 1A and 1B reached 215.30 metres and 379.40 metres respectively, penetrating aeolian sands overlying the Bulldog Shale, Cadna-owie Formation an d Observatory Hill Beds. In contrast to Byilkaoora 1, oil shows and calcite pseudomorphs after...
Marla 1A and 1B reached 215.30 metres and 379.40 metres respectively, penetrating aeolian sands overlying the Bulldog Shale, Cadna-owie Formation an d Observatory Hill Beds. In contrast to Byilkaoora 1, oil shows and calcite pseudomorphs after evaporite minerals (shortite and trona) are absent and a 2-fold stratigraphic subdivision is recognised. A playa lake model has been proposed for the Cambrian sequence in Byilkaoora 1, but a marine depositional environment is here suggested for the Marla 1A and 1B carbonates; a NE-oriented, low-lying land barrier may have separated the two areas during the Cambrian.
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