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Deep Sea Research Part A. Oceanographic Research Papers, 1979
Abstract Interstitial methane profiles from six sediment cores taken on the slope and abyssal plain of the Gulf of Mexico can be explained by simple kinetic modeling. Methane is apparently produced at a constant rate and microbially consumed in the sulfate-reducing zone.
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Abstract Interstitial methane profiles from six sediment cores taken on the slope and abyssal plain of the Gulf of Mexico can be explained by simple kinetic modeling. Methane is apparently produced at a constant rate and microbially consumed in the sulfate-reducing zone.
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The Mineralogy of Marine Sediments
1989Those grains that were originally formed on the continents and have subsequently been transported into the ocean. River transport is the most important mechanism in which terrigenous minerals are passed to the ocean realm. Milliman & Meade (1983) estimate that about 12–13 × 109 tonnes of suspended sediment are supplied to the oceans by rivers annually ...
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Gas in Marine Sediments—an introduction
Marine Geology, 1997vanWeering, TCE, Klaver, GT, Prins, RA
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