The Canadian Mineralogist; February 2009; v. 47; no. 1;
p. 39-51; DOI: 10.3749/canmin.47.1.39
© 2009 Mineralogical Association of Canada
YUKONITE FROM THE GROTTA DELLA MONACA CAVE, SANTAGATA DI ESARO, ITALY: CHARACTERIZATION AND COMPARISON WITH COTYPE MATERIAL FROM THE DAULTON MINE, YUKON, CANADA
Anna Garavelli1,
Daniela Pinto1,
Filippo Vurro1,
,
Marcello Mellini2,
Cecilia Viti2,
Tonci Bali
-
uni
3 and
Giancarlo Della Ventura4
1 Dipartimento Geomineralogico, Università di Bari, Via E. Orabona 4, I–70125 Bari, Italy
2 Dipartimento di Scienze della Terra, Università di Siena, Via Laterina 8, I–53100 Siena, Italy
3 Department of Geography and Geology, University of Copenhagen, Øster Volgade 10, DK-1350 Copenhagen K, Denmark
4 Dipartimento di Scienze Geologiche, Università di Roma Tre, Largo S. Leonardo Murialdo 1, I-00146 Rome, Italy

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FIG. 2. (a) Back-scattered electron microphotograph of the Grotta della Monaca yukonite, showing dehydration-induced fractures, and (b) a granular texture, with close association of bright and dark grains.
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FIG. 3. (a) TEM image of the Grotta della Monaca yukonite, showing grains finely intermixed with an amorphous matrix; (b) irregular, bent and polygonized lattice fringes.
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FIG. 4a. Unpolarized single-crystal FTIR spectra of yukonite from the Daulton mine, Yukon, Canada, and from Grotta della Monaca cave, collected on randomly oriented ~30 mm thick fragments.
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FIG. 4b. High-temperature FTIR spectra of yukonite from Grotta della Monaca. Temperature in °C. On the left side, the 2000–1000 cm–1 range is magnified for clarity.
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FIG. 6a. X-ray powder-diffraction patterns of yukonite from Grotta della Monaca (G) and Venus mine (V), Yukon Territory, Canada (ROM sample no. M37256, kindly placed at our disposal by the Royal Ontario Museum of Toronto). The sample from Grotta della Monaca contains some scorodite, whereas the one from the Venus mine has no additional phases.
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FIG. 6b. X-ray powder-diffraction patterns of yukonite from the Daulton mine with quartz. CuK 1 radiation, Guinier geometry. The background has been subtracted, and diagrams have been smoothed.
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Copyright © 2010 by Mineralogical Association of Canada