Towards Reconciling Early Solar System Chronometers: The 238U/235U Ratios of Chondrites and D'Orbigny Pyroxenes

Physics

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Scientific paper

A new 238U/235U ratio for the pyroxene fraction of the D'Orbigny angrite
adjusts the previously reported Pb-Pb age of -0.6±0.3 Ma.
This adjustment affects all short-lived chronometers anchored to
D'Orbigny and reconciles some discrepancies in early solar system
materials.

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