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In the re-evaluation of previous studies it was found that 'Maghagendorfite is absent from the samples, since the cationic distribution used here considers a preference of Mg for the M(2) site, not for M(1).' He concluded that 'since the cationic distribution of maghagendorfite is unlikely, we recommend considering this species as “Questionable”.'","1978","8","A","C","10","38","2","3","4","Monoclinic",5,"0","Space Group: n.d. Z = n.d.",4.5,"Translucent","greenish black",[47,48],"black","green","Good on {001}; poor on {110} (by analogy to hagendorfite)","Distinct\u002FGood","Biaxial","complex zoned granite pegmatite.","This root name is a series in the Alluaudite Group. The species maghagendorfite-Na□ was originally found at the Dyke Lode granite pegmatite in the Keystone District, Pennington Co., South Dakota (Moore and Ito, 1979). Maghagendorfite-NaNa was later fou...","Named by Paul (Paulus) Brian Moore and Jun Ito in 1979 for magnesium and the relationship to hagendorfite. 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