(Table 5) Average organic carbon accumulation rates in the Argo and Gascoyne abyssal plains
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The table was assembled using constant sedimentation rate intervals (Ludden, Gradstein, et al., 1990, doi:10.2973/odp.proc.ir.123.1990) and the average TOC (calculated from all Rock-Eval data, Ludden, Gradstein, et al., (1990)) in that interval. A porosity of 50% and a grain density of 2.6 was used for all calculations.
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2025-11-03
