Fig. 6From: Formation of ferroan dacite by lunar silicic volcanism recorded in a meteorite from the Moona Al versus Ti and b Fe# versus Ti# in pyroxenes from the silicic clast (this work). Compositions of ARFe clasts in NWA 773 (Fagan et al. 2014), NWA 2977 OG (Nagaoka et al. 2015), and 15405 QMD (56, 145) (Fagan et al. 2014) are also shownBack to article page