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Carbonate cements mixed marine-meteoric water

Figure 8.16. A hypothetical trend of changes in the stable isotope composition of carbonate cements in different diagenetic environments. A- marine realm B-meteoric realm C- mixing zone D- successively deeper burial for calcite spar E-successively deeper burial for saddle dolomite. B through E are precipitated in progressively hotter waters. (After Choquette and James, 1987.)... Figure 8.16. A hypothetical trend of changes in the stable isotope composition of carbonate cements in different diagenetic environments. A- marine realm B-meteoric realm C- mixing zone D- successively deeper burial for calcite spar E-successively deeper burial for saddle dolomite. B through E are precipitated in progressively hotter waters. (After Choquette and James, 1987.)...
See other pages where Carbonate cements mixed marine-meteoric water is mentioned: [Pg.9]    [Pg.11]    [Pg.285]    [Pg.406]    [Pg.33]    [Pg.380]    [Pg.4]    [Pg.204]    [Pg.370]   


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Carbon marine

Carbon mix

Carbonate cements

Carbonated waters

Cements Mixed

METEOR

Marine water

Marine-carbonate

Meteorism

Mixing water

Water carbon)

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