The structure of wodginite (non-centrosymmetric monoclinic space group Cc; ideal formula, MnX1X2Tao2 where site X2 contains 5-valent ions (and all the niobium) and the average valency of cations in site X1 is 4) was determined by film methods to be an ordered form of the ixiolite structure. The a and b cell edges and angle β increase with manganese content, whereas c remains constant for wodginites from five localities in Western Australia.

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