Sulfate-methane transition as a proxy for average methane hydrate saturation in marine sediments-Reference-Cited by-同舟云学术

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Sulfate-methane transition as a proxy for average methane hydrate saturation in marine sediments

Published:2008-02-08 Issue:3 Volume:35 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Bhatnagar Gaurav,Chapman Walter G.,Dickens Gerald R.,Dugan Brandon,Hirasaki George J.

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference16 articles.

1. Early Diagenesis

2. Generalization of gas hydrate distribution and saturation in marine sediments by scaling of thermodynamic and transport processes;Bhatnagar;Am. J. Sci.,2007

3. Marine pore-water sulfate profiles indicate in situ methane flux from underlying gas hydrate;Borowski;Geology,1996

4. Global and local variations of interstitial sulfate gradients in deep-water, continental margin sediments: Sensitivity to underlying methane and gas hydrates;Borowski;Mar. Geol.,1999

5. Methane and other hydrocarbon gases in marine sediment;Claypool;Annu. Rev. Earth Planet. Sci.,1983

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