Author:
Plimer I. R.,Ashley P. M.
Abstract
SummaryManganoan ilvaite forms as an early retrograde metamorphic phase from calcic rhodonite in the polymetamorphosed Pb-Zn sulphide/manganese silicate rocks at Broken Hill and from grossular-andradite in a skarn at Ban Ban. Ilvaite exists as a probable metastable phase into which Mn is apparently strongly partitioned. The manganoan ilvaites analysed contain up to 13·5 % MnO substituting for FeO and this substitution shifts the 020 peak.
Subject
Geochemistry and Petrology
Cited by
13 articles.
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1. INESITE, HUBEITE, RUIZITE, APOPHYLLITE, AND MANGANOAN ILVAITE FROM CAVNIC, EASTERN CARPATHIANS, ROMANIA;Carpathian Journal of Earth and Environmental Sciences;2022-08-31
2. Ecandrewsite (ZnTiO3) in Amphibolites, Sierras de Córdoba, Argentina: Mineral Chemistry and Comparison with Different Worldwide Paragenetic Occurrences;The Canadian Mineralogist;2022-07-01
3. Ilvaite as a thermodynamic recorder of multistage retrograde alteration in large Galinge skarn Fe deposit, western China;Journal of Central South University;2019-12
4. Formation and Breakdown of Ilvaite in the Large Galinge Skarn Fe Deposit, Western China: A Record of Multistage Retrograde Alteration;Springer Theses;2019
5. Ilvaite stability in skarns from the northern contact of the Maladeta batholith, Central Pyrenees (Spain);European Journal of Mineralogy;2010-06-23