Ximengite is a very rare bismuth phosphate, formed through the alteration of Bi-bearing sulfides and sulfosalts. It was discovered in the tin mining district of the Ximeng County (Yunnan, China) in 1989. Recently this mineral species was also identified in the hydrothermal veins from Fornovolasco (Apuan Alps, Tuscany, Italy), in white earthy masses, associated with mimetite and bismutite, originated by the alteration of bismuth-bearing sulfides or sulfosalts
Ximengite, a new occurrence from Apuan Alps (Tuscany, Italy)
BIAGIONI, CRISTIAN;PERCHIAZZI, NATALE;
2010-01-01
Abstract
Ximengite is a very rare bismuth phosphate, formed through the alteration of Bi-bearing sulfides and sulfosalts. It was discovered in the tin mining district of the Ximeng County (Yunnan, China) in 1989. Recently this mineral species was also identified in the hydrothermal veins from Fornovolasco (Apuan Alps, Tuscany, Italy), in white earthy masses, associated with mimetite and bismutite, originated by the alteration of bismuth-bearing sulfides or sulfosaltsFile in questo prodotto:
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