Assertion: aquifer's brine | /r/CapableOf | evolve dolomitization
Facets:
value: through aragonite
type: LOCATION
value: through calcite
type: MANNER
Source sentences:
text: The Sr/Ca ratios (0.03–0.17) of the produced waters from Marcellus wells are significantly higher than brines evolved through calcite (0.4–1.6·10-3) or aragonite (1.5–2.2·10-2) dolomitization but are consistent with equilibrium with other minerals such as gypsum or celestite (27).