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European Journal of Mineralogy; April 2002; v. 14; no. 2; p. 375-377; DOI: 10.1127/0935-1221/2002/0014-0375
© 2002 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Articles

The anhydrous amphibole ungarettiite from the Woods mine, New South Wales, Australia

Yosuke KAWACHI1,*, Douglas S. COOMBS1,**, Bernard E. LEAKE2 and Richard W. HINTON3

1 Geology Department, University of Otago, Dunedin, New Zealand
* Current address: Yukari Ichibangai 2–408, Izumicho 3 Chome16Kokubunji185-0024, Japan
2 Department of Earth Sciences, Cardiff University, PO Box 914, Cardiff, CF1 3YE, Wales, United Kingdom
3 Department of Geology and Geophysics, University of Edinburgh, West Mains Road, Edinburgh, EH9 3JW, Scotland, United Kingdom

** Corresponding author, e-mail: doug.coombs{at}stonebow.otago.ac.nz

We report ungarettiite from the Woods mine, New South Wales, Australia; this is the second known occurrence. Electron-microprobe and ion-probe analyses show it to be very close to end-member composition, NaNa2Mn2+2Mn3+3Si8O22O2. We record the first direct determination of H2O (<60ppm) in this anhydrous amphibole, together with F (53ppm) and Cl (5ppm), giving (OH+F+C1) a maximum of~0.01 sites per formula unit. Li, ~4 ppm, and other trace elements are reported, most of them for the first time. Like various associated minerals, it contains very low to negligible Al, Mg, and Ca. Fe varies from below detection by EMP analysis to about 0.35 atoms p.f.u. Fe is strongly partitioned into any associated manganian aegirine.

Key-words: ungarettiite, amphibole, Woods mine, manganese mineral, ion-probe analyses.




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