First-principles estimates of equilibrium magnesium isotope fractionation in silicate, oxide, carbonate and hexaaquamagnesium(2+) crystals

274 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Planetary and meteoritic Mg/Si and δ30Si variations inherited from solar nebula chemistry (2015, methodology): “Based on spectroscopic data and first principle calculations, the equilibrium fractionation factors between forsterite-Mggas (Huang et al., 2013; Schauble, 2011) and”
First-principles calculations of equilibrium Mg isotope fractionations between garnet, clinopyroxene, orthopyroxene, and olivine: Implications for Mg isotope thermometry (2013, methodology): “Furthermore, as the theoretical calculations show, substitution of Al3þ , Cr3þ , and Fe3þ in the octahedral site of the spinel can cause significant variations of 1000lnb26–24 even at temperature up to 1000 K (Schauble, 2011).”