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Abstract
Bulletin of Canadian Petroleum Geology
Vol. 11 (1963), No. 4. (December), Pages 389-395
Paleocurrent Directions From the McMurray Formation
M. A. Carrigy
ABSTRACT
The paleoslope during the deposition of the McMurray Formation was north ward. Measurement of 481 high-angle planar cross-beds gives a vector mean direction of 350 degrees and a mean dip of 25.13 degrees.
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