Research Article
Multiple Controls on the Accumulation of Organic-Rich Sediments in the Besa River Formation of Liard Basin, British Columbia, Canada
Figure 9
MoEF versus UEF in wells (a) A-038-B/94-N-08, (b) B-023-K/94-O-05, and (c) B-003-K/94-O-12. Dotted lines indicate Mo/U molar ratios as multiples of the seawater value (3x SW, 1x SW, 0.3x SW, and 0.1x SW) (modified from Algeo and Tribovillard [24]).
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