| http://www.w3.org/ns/prov#value | - Of course, if other information regarding the quantity of dolomite, calcite, and other carbonates is known (such as via a neutron-density cross-plot), the analysis at 224 and 226 may be unnecessary as the excess calcium due to the anhydrite/gypsum may be found by subtracting the calcium in dolomite, calcite, etc. from the total detected calcium.
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