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BUL 030

Petrographic and Engineering Properties of Fine Grained Rocks of Central Alberta

The central Alberta Plains are underlain by a gently westward-dipping succession of non-marine detrital strata of Late Cretaceous and Paleocene ages, which merges to the west with folded and faulted retaceous beds of the Rocky Mountain ... Show Abstract

Locker, J.G.  1973-01-01

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