Strontium Isotope Ratios for an Igneous Rock Sample
| Stage | Ratio |
|---|---|
| Crystal core | = 0.71685 |
| Crystal rim | 0.71548 |
| Crystal matrix | 0.71416 |
A student is studying igneous rock formations on Elba Island, Italy, and reviews published data on the ratio of strontium isotopes () in minerals from a specific rock sample. These isotope ratios provide information about the composition of the magma that formed the rock. Ratios below 0.710 suggest more material from the mantle in the magma, while ratios increasing above that number usually indicate greater proportions of material from the continental crust. The minerals in the rock sample record three growth stages: crystal core zones formed first, then rim zones, and finally the surrounding matrix. The student concludes that the rock sample