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The latitudinal trend in the mid-Cretaceous isotopic values is interpreted to be the result of an intensified hydrologic cycle, and has been quantified with a stable isotope mass-balance model. Therefore, the mass-balance calculations that are required to be reported by complying companies are most often just educated guesstimates, the accuracy of which can never be verified. Green sands must be controlled compositionally based on the mass-balance system, as is done in melting. |
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