Abstract:The Carboniferous Lisburne Group, a succession of carbonate rocks, has been identified in the Brooks Range Endicott Mountains allochthon, parautochthonous rocks in the northeastern Brooks Range, and in the North Slope subsurface. The Lisburne Group was the original reservoir exploration target in the Lisburne field at Prudhoe Bay. Its importance as both a potential subsurface source and reservoir rock warrants further investigation into the carbonate facies, lithologies, and conodont microfacies for continued … Show more
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