Abstract
Sediments deposited in the Indus Fan (Site 720) as well as Miocene sediments from the Owen Ridge (Sites 722 and 731) contain almost exclusively organic matter of terrigenous origin. The organic matter in sediments from the Oman Margin (Sites 723, 725, and 728) and in the Pliocene/Pleistocene sections from the Owen Ridge is mainly of a marine origin with variable admixtures of terrigenous material. -from Authors
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CITATION STYLE
APA
Ten Haven, H. L., & Rullkotter, J. (1991). Preliminary lipid analyses of sediments recovered during Leg 117. Proc. Scientific Results, ODP, Leg 117, Oman Margin/Neogene Package, 561–569. https://doi.org/10.2973/odp.proc.sr.117.160.1991
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