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Dipartimento di Scienze della Terra, Università di Pisa, Via S. Maria 53, I-56126 Pisa, Italy, pasero@dst.unipi.it
| The first 20% of the full text of this article appears below. |
| INTRODUCTION |
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Starting from the basic formula of manganese dioxide, Mn4+O2, incorporation of mono- and divalent cations (primarily alkali and alkali earths) within the tunnels of the structures, can be accommodated by partial reduction of manganese. Until recently, there was a considerable uncertainty and lively debate (e.g., Burns et al. 1983; Burns et al. 1985; Giovanoli 1985) concerning the valence of the reduced species and whether Mn2+ or Mn3+ was present. It is now commonly accepted on the basis of several high-quality structural studies that Mn3+ replaces Mn4+. In titaniferous phases, charge balance accompanying the inclusion of tunnel cations is not adjusted by reduction to Ti3+, but through incorporation of Fe3+, V3+ or Cr3+ substituting for Ti4+. The generic substitutions can be summarized in the generic formula:
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where
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