Ecandrewsite – Zincian Pyrophanite from Lujavrite, Pilansberg Alkaline Complex, South Africa

نویسندگان

  • ROGER H. MITCHELL
  • RUSLAN P. LIFEROVICH
چکیده

Ilmenite-group titanates are relatively common accessory minerals in agpaitic nepheline syenite (lujavrite) in the Pilansberg alkaline complex, South Africa. They crystallized in three generations and form a continuous ecandrewsite – pyrophanite solidsolution extending from (Zn0.81Mn0.12Fe0.07)TiO3 to (Mn0.93Fe0.7)TiO3. The earliest generation of ferroan manganoan ecandrewsite of widely varying composition (Zn0.81–0.53Mn0.33–0.12Fe0.11–0.04)TiO3 is replaced by zincian pyrophanite (Mn0.82–0.34Zn0.50– 0.20Fe0.13–0.06)TiO3. The latest generation is pyrophanite with only traces of zinc, showing a compositional evolution toward ferroan pyrophanite. The three generations of Zn–Mn titanates recognized on the basis of their paragenesis and composition crystallized during the subsolidus alteration of the lujavrite by evolving deuteric alkaline fluids. The enrichment in Zn, Mn, and Ti in these fluids resulted from the decomposition of earlier-formed magmatic-stage Znand Mn-bearing titanoand zirconosilicates. This is the first reported occurrence of a near-complete ecandrewsite – pyrophanite (ZnTiO3 – MnTiO3) solidsolution series.

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تاریخ انتشار 2004