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Thermochemical sulphate reduction

Machel, H.-G. (1987) Saddle dolomite as a by-product of chemical compaction and thermochemical sulphate reduction. Geology, 15, 936-940. [Pg.360]

Manzano B.K., Fowler M.G., Machel H.G. (1997) The influence of thermochemical sulphate reduction on hydrocarbon composition in Nisku reservoirs, Brazeau river area, Alberta, Canada. Org. Geochem. 21, 507-21. [Pg.347]

Fig. 9. Decreasing values of SF(C3-nC5) accompanied by increasing levels of H2S in gas-condensates are attributed to thermochemical sulphate reduction. Concomitant increase in SF(C3- Cs) and H2S in oils is postulated to be due to admixture of H2S-bearing gas-condensate. Fig. 9. Decreasing values of SF(C3-nC5) accompanied by increasing levels of H2S in gas-condensates are attributed to thermochemical sulphate reduction. Concomitant increase in SF(C3- Cs) and H2S in oils is postulated to be due to admixture of H2S-bearing gas-condensate.
Krouse, H. R., Viau, C. a., Eliuk, L. S., Ueda, A. Halas, S. 1988. Chemical and isotopic evidence of thermochemical sulphate reduction by light hydrocarbon gases in deep carbonate reservoirs. Nature, 333, 415-419. [Pg.25]

See other pages where Thermochemical sulphate reduction is mentioned: [Pg.161]    [Pg.161]    [Pg.15]    [Pg.161]    [Pg.161]    [Pg.15]    [Pg.82]   
See also in sourсe #XX -- [ Pg.15 , Pg.271 , Pg.272 , Pg.275 ]



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Sulphate reduction

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