Comment on “Valence state of titanium in the Wark–Lovering rim of a Leoville CAI as a record of progressive oxidation in the early Solar Nebula” by K.A. Dyl, J.I. Simon and E.D. Young

Dyl et al. (2011) state that their results confirm the conclusion of J. Simon et al. (2005) that the pyroxene in Wark–Lovering rims (Wark and Lovering, 1977) found on Ca-, Al-rich refractory inclusions has lower Ti3+/Titot ratios than the primary pyroxene in the interiors of inclusions. While true,...

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Veröffentlicht in:	Geochimica et cosmochimica acta 2012-05, Vol.85 (5, 2012), p.373-376
Hauptverfasser:	Simon, S.B., Grossman, L., Sutton, S.R.
Format:	Artikel
Sprache:	eng
Schlagworte:	calcium GEOSCIENCES OXIDATION SILICATE MINERALS SOLAR NEBULA TITANIUM VALENCE
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