Organic carbon, reduced sulfur, and iron in miocene to holocene upwelling sediments from the Oman and Benguela upwelling systems.
المصدر
Proc. scientific results, ODP, Leg 117, Oman Margin/Neogene package, p. 517-527
الناشر
ODP, Texas A&M University College Station.
الملخص الإنجليزي
Sedimentary pyrite formation in upwelling sediments is limited by an as yet unknown factor, and caution is advised in using C/S ratios and C vs. S diagrams in paleoenvironmental reconstructions for organic-rich sediments.
المعرف
DOI: 10.2973/odp.proc.sr.117.155.1991
