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Abstract
Bulletin of Canadian Petroleum Geology
Vol. 11 (1963), No. 3. (September), Pages 267-287
Ghost River Type Section
J. D. Aitken
ABSTRACT
The Main Ranges Cambrian succession is recognizable in the Ghost River type section; the name "Ghost River" is therefore redundant. Pre-Fairholme Devonian rocks, largely detrital red beds, are very thin at the "Ghost River" type section, but thicken considerably in a sub-Devonian channel nearby.
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