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This therefore allows crustal formation ages to be calculated, despite any metamorphism the sample has undergone.

It is useful to geologists and archaeologists who want to know when such an event occurred.They have relatively homogeneous trace-element signatures, and therefore their isotopic evolution can model the evolution of the whole Solar system and of the "bulk Earth".After plotting the ages and initial Nd ratios of terrestrial igneous rocks on a Nd evolution vs.Nd ratios of the samples analyzed are plotted on a ɛNd versus time diagram shown in the figure.De Paolo (1981) fitted a quadratic curve to the Idaho Springs and average ɛNd for the modern oceanic island arc data, thus representing the neodymium isotope evolution of a depleted reservoir.

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