☢️ Isotope Dating

Calculated age—
Age uncertainty ±—
Half-lives elapsed—
Concordance—
Radioactive Decay
N(t) = N₀·e−λt
t = −ln(N/N₀)/λ
t½ = ln2/λ
U-Pb concordia: plot ²⁰⁷Pb/²³⁵U vs ²⁰⁶Pb/²³⁸U — concordant samples lie on Wetherill curve.

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