The 146,147Sm-142,143Nd Chronometer and the Timescales of Early Planetary Differentiation

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Scientific paper

Complexities in the 146,147Sm-142,143Nd system of Earth, Mars and the
Moon suggest that igneous rocks that sample their mantles were derived
from mixtures due to mantle convection and that simple static models of
magma ocean layers in the lunar and martia

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