Use this geological calculation for a transparent first-pass interpretation of measured rock, soil, fluid, well, stratigraphic, isotopic, geophysical, or seismic data under an explicitly selected model.

Measured 87Sr/86Sr

Measured (uncorrected) 87Sr/86Sr ratio.

Measured 88Sr/86Sr

Measured 88Sr/86Sr used to estimate mass bias.

Correct a measured 87Sr/86Sr ratio for instrumental mass bias by exponential-law normalization to 88Sr/86Sr = 8.375209. The tool evaluates the supplied inputs together and returns the named outputs below; it does not infer omitted operating conditions or change the units shown.^[1]

Beta

Exponential-law mass bias coefficient per amu.

Corrected 87Sr/86Sr

Mass-bias-corrected true 87Sr/86Sr ratio.

• Radiometric ages require the correct decay constants, isotopic ratios, standards, common-component correction, closure interpretation, initial composition, and analytical uncertainties. Disturbance, inheritance, diffusion, alteration, and model choice can make a calculated number differ from the geological event age.
• Use finite inputs in the displayed units and preserve more precision than the final presentation requires. Independently verify safety-critical, financial, compliance, or production decisions.

Compare independent measurements and models, retain units and analytical metadata, propagate uncertainty, and validate interpretations against logs, cores, maps, laboratory data, or field observations.

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