Document
Organic carbon, reduced sulfur, and iron in miocene to holocene upwelling sediments from the Oman and Benguela upwelling systems.
Identifier
DOI: 10.2973/odp.proc.sr.117.155.1991
Source
Proc. scientific results, ODP, Leg 117, Oman Margin/Neogene package, p. 517-527
Contributors
Morse, John W., Author
Mays, Linda L., Author
Country
United States.
City
Texas
Publisher
ODP, Texas A&M University College Station.
Gregorian
1991-02-01
Language
English
Subject
English abstract
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.
Category
Journal articles
File size
2.37 MB
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