Olivine grain boundaries in undeformed basalts are ~1 nm crystalline interfaces that selectively store Ca, Al, P, Na and Ti, with Ca coverage matching near-magmatic equilibrium segregation.
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Nanoscale Storage of Incompatible Elements at Olivine Grain Boundaries in Natural Basalts
Olivine grain boundaries in undeformed basalts are ~1 nm crystalline interfaces that selectively store Ca, Al, P, Na and Ti, with Ca coverage matching near-magmatic equilibrium segregation.