Is so-called Al-Mg isochron for a meteorite CAI a two component mixing line?

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Internal Al–Mg isotope systematics of a Type B CAI: Remelting of refractory precursor solids

High precision SIMS Al–Mg isotope analyses were performed for a pristine Type B1 CAI Leoville 3535-1 on multiple mineral phases that include aluminum-rich zoned melilite mantle (Åk20–Åk60), magnesium-rich melilite (Åk70), fassaite, spinel and anorthite in the core. The data yield a well-defined internal isochron with an inferred initial Al/Al ratio of (5.002 ± 0.065) 10 , which is lower than th...

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ژورنال

عنوان ژورنال: GEOCHEMICAL JOURNAL

سال: 1985

ISSN: 0016-7002

DOI: 10.2343/geochemj.19.223