Slides to Chapter D
Ore deposits in mafic and ultramafic intrusive rocks, without alkaline rocks
Example : Chromite deposit, Ni-PGE in layered mafic intrusions
Schatter cones in Huronian Quartzites at Sudbury, Canada
Shatter cones are conical fractures typical of rocks having been subjected to shock.
In the case of Sudbury, they have been attributed to a meteorite impact.
Photo: LluÃs Fontboté, 1999.09.09/03
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Chromite "Schlieren" in the ultramafic body of Ronda. Photo: LluÃs Fontboté, 2000.0./321
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Massive Chromite (Ni-Cu) vein in the Baeza mine, Ojén Massif, Ronda. The Los Jarales polished section pictured in this polished section comes from a nearby similar deposit. Photo LluÃs Fontboté 2005.05/65
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Chromite, Fe+2Cr2O4, a spinel
Sawn slab (10x9 cm) of orbicular chromite, typical for podiform chromite deposits.
DoÄŸanbaba-YeÅŸilova, Burdur, Turkey
© Photo and coll. P. Perroud