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colored shale, siltstone, and sandstone, appear to be tightly folded and locally thrust faulted. These sediments were intruded in the Lower Cretaceous by the calc-alkaline plutons of the Lassiter Coast Intrusive Suite. N
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Document Date: 2011-05-06 04:09:14
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colored shale, siltstone, and sandstone, appear to be tightly folded and locally thrust faulted. These sediments were intruded in the Lower Cretaceous by the calc-alkaline plutons of the Lassiter Coast Intrusive Suite. N