Multiple Controls on the Accumulation of Organic-Rich Sediments in the Besa River Formation of Liard Basin, British Columbia, Canada

<div>Major elemental distributions of Al2O3 versus K2O, TiO2, and CaO, and Zr versus Al2O3+K2O+TiO2 in wells (a) A-038-B/94-N-08, (b) B-023-K/94-O-05, and (c) B-003-K/94-O-12.</div>

Geofluids

fig7

Figure 7

Figure 7: Multiple Controls on the Accumulation of Organic-Rich Sediments in the Besa River Formation of Liard Basin, British Columbia, Canada 