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European Journal of Mineralogy; June 2001; v. 13; no. 3; p. 605-610; DOI: 10.1127/0935-1221/2001/0013-0605
© 2001 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Lead-antimony sulfosalts from Tuscany (Italy). III. Pillaite, Pb9Sb10S23ClO0.5, a new Pb-Sb oxy-chloro-sulfosalt, from Buca della Vena mine

Paolo ORLANDI1,*, Yves MOËLO2, Alain MEERSCHAUT2 and Pierre Palvadeau2

1 Dipartimento di Scienze della Terra, Università di Pisa, Via S. Maria 53, I-56126 Pisa, Italy
2 Laboratoire de Chimie des Solides, Institut des Matériaux J. Rouxel, UMR CNRS 6502, 2 rue de la Houssinière, 44322 Nantes Cedex 3, France


Figure 1
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Fig. 1. Scanning electron microscope image of pillaite fibers.

 

Figure 2
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Fig. 2. Reflectance curves of pillaite in air and oil.

 

Figure 3
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Fig. 3. Bragg photograph obtained by rotation along the elongation axis b on pillaite single crystal, hkl indexing according to the weak 2b superstructure.

 

Figure 4
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Fig. 4. Projection along b of the crystal structure of pillaite (half unit cell a/2 x c). In order of decreasing size: Pb (medium grey), (Pb, Sb) (cross-hatched), Sb (light grey), Cl (light grey), S (white) and O (black). Oxygen position is half-filled.

 





JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
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