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ated surfaces suggest deposition from wet-based terrestrial glaciers. Black shales of the overlying Mackellar Formation are in sharp contact with diamictite and sandstone of the Pagoda Formation. Lonestones are extremely
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Document Date: 2011-05-06 17:37:20
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ated surfaces suggest deposition from wet-based terrestrial glaciers. Black shales of the overlying Mackellar Formation are in sharp contact with diamictite and sandstone of the Pagoda Formation. Lonestones are extremely