Regionally extensive, pre-Pennsylvanian, meteoric zoned calcite cements from the Mississippian age Lake Valley Formation (New Mexico) comprise three major zones, zones 1, 2, and 3, each with a distinct isotope and trace element geochemistry. Zone 1 has the highest Mg, 18O, and 13C contents, zone 2 intermediate values and greatest Mn and Fe, and zone 3 has the lowest trace element, 18O, and 13C values. Covariation of C and O isotopes for the three zones define an inverted “L”-shaped trend, and covariations of Mg-Mn and Mg-Fe define “L”-shaped trends, all suggestive of rock evolution curves resulting from water-rock interaction. These covariant trends were the impetus for quantitative mass balance modelling of water-rock interaction. Iterative mass balance modelling of covariations of stable isotopes (C and O) and trace elements (Mg, Mn, Fe) of these zoned cements implies that water-rock interaction progressively decreased (water/rock ratios increased) during precipitation. Cementing waters for the oldest cement zone (zone 1) resulted from water/rock ratios in the range of tens to a few hundred, whereas the youngest cement (zone 3) resulted from water/rock ratios in the 100's to 1000's. The modelling also implies that differences in geochemistry of the cement zones cannot be explained solely by changes in water/rock ratios, but require greater 18O, and greater Ca and Mg concentrations in input waters that evolved to zone 1 precipitational waters than those for zones 2 and 3. Zones 2 and 3 can reasonably be modelled using input waters with the same isotopic compositions, the same Ca concentration, and for some zone 2 cement the same Mg concentrations. The minimum Mg/Ca ratios in input waters is constrained by the lower Mg “plateau” in Mg-Mn space, and is about the same for all three zones, about 1/25. The maximum Mg/Ca ratios (about 1 20 ) occurred in zone 2 input waters. Mn-Fe covariations also show an “L”-shaped trend, a trend whch fits neither a simple water-rock interaction model, nor a simple Eh model. A model is proposed in which Eh and limited Mn sources determine the amount of Fe and Mn available in solution to partake in water-rock interaction. Water-rock interaction modelling provides one useful approach to quantitatively interpreting isotopic and trace element data from diagenetic carbonates to gain a clearer understanding of evolution of diagenetic fluids.
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