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Abstract
Bulletin of Canadian Petroleum Geology
Vol. 13 (1965), No. 2. (June), Pages 271-279
Source of the Allenby Formation, Princeton Coalfield, British Columbia
L. V. Hills
ABSTRACT
Detailed studies of cross-stratification, pebble imbrication, mineralogy, textures, phenoclast size, and individual mineral size all indicate a single paleocurrent direction within the Tertiary Allenby Formation. It is concluded that the paleocurrents were in a southerly direction, and that the main source of the sediments was the Osprey Lake Intrusion.
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