Seventy-one samples from nine sites were analyzed for total organic carbon (TOC). Fifty-six samples, containing 0.2% or more TOC, were evaluated by Rock-Eval to assess the nature of their kerogen and its petroleum source potential. Visual kerogen studies were carried out. Petroleum potential was encountered only in Valanginian calcareous claystones at Hole 692B close to the margin of Dronning Maud Land. Kerogens in Eocene to Pliocene sediments of the central and western Weddell Sea (Sites 694, 695, 696, and 697) are similar everywhere, largely comprising brown to black, granular, amorphous material of high rank, and generally possessing several reflectance populations of vitrinite particles. The latter are interpreted as indicative of the recycling of sediments of a variety of levels of thermal maturity. -from Authors
CITATION STYLE
Thompson, K. F. M., & Dow, W. G. (1990). Investigation of Cretaceous and Tertiary kerogens in sediments of the Weddell Sea. Proc., Scientific Results, ODP, Leg 113., Weddell Sea, Antarctica, 189–197. https://doi.org/10.2973/odp.proc.sr.113.164.1990
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