Abstract
At both sites, organic carbon content is low in the Eocene samples (0.10 to 0.20%) and relatively high in the Pliocene/Miocene samples (0.87 to 1.15%). The Maestrichtian samples from Site 612 contain about 0.6% organic carbon. The organic matter is predominantly terrigenous, as indicated by low hydrogen index values from Rock-Eval pyrolysis and the dominance of long-chain wax alkanes in the extractable hydrocarbons.-from Authors
Cite
CITATION STYLE
Stein, R., Rullkotter, J., Kalkreuth, W., & Welte, D. H. (1987). Quantity, provenance, and thermal maturity of organic matter from the New Jersey continental margin, Deep Sea Drilling Project, Leg 95. Initial Reports DSDP, Leg 95, St. John’s to Ft. Lauderdale, 651–659. https://doi.org/10.2973/dsdp.proc.95.128.1987
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.