Geology, v. 43, p. 935–938, doi:10.1130/G37082.1

In the second paragraph of the introduction, there is an editing error (shown in bold) in the following sentence:

For forsterite contents [Fo = 100 × Mg/(Mg + Fe)] between 60% and 90%, the diffusivity of Fe-Mg along the c crystallographic axis varies between 0.1 m2/s and 1 × 10–15m2/s [Dohmen et al., 2007; assuming oxygen fugacity, ƒO2, near the quartz-magnetite-fayalite buffer (QFM), pressure, P = 0.1 MPa, and temperature, T = 1200 °C].

The correct version of the sentence should read:

For forsterite contents [Fo = 100 × Mg/(Mg + Fe)] between 60% and 90%, the diffusivity of Fe-Mg along the c crystallographic axis varies between 0.1 × 10–15m2/s and 1 × 10–15m2/s [Dohmen et al., 2007; assuming oxygen fugacity, ƒO2, near the quartz-magnetite-fayalite buffer (QFM), pressure, P = 0.1 MPa, and temperature, T = 1200 °C].