Abstract
Material of continental origin constitutes a considerable fraction of the organic matter in the sediments investigated. The contribution of terrigenous material varied with time with high levels corresponding with turbidites. It appears that organic matter transported from the continent by turbidity flows was subjected to a kind of physico-chemical fractionation during which it was enriched in spore and pollen material. This means that the dispersed organic matter is predominantly lipoid. - from Authors
Cite
CITATION STYLE
Galimov, E. M. (1980). A study of organic matter from deep oceanic bore holes, Deep Sea Drilling Project sites 415 and 416, in the Moroccan Basin. Initial Reports of the Deep Sea Drilling Project, Leg 50, Funchal, Madeira Islands, 1976, (U. S. GPO; U. K. Distributors IPOD Committee, NERC, Swindon), 575–603. https://doi.org/10.2973/dsdp.proc.50.120.1980
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
