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Dolomite — specimens [gallery view]

Formed by diagenesis or hydrothermal metasomatism of limestone; a major component of some contact metamorphic rocks and marbles; a gangue in hydrothermal veins; in carbonatites and ultramafic rocks (Anthony et al., 2001—2005). Faceted specimens are very rare.
Dolomite — specimen 0165

Dolomite — specimens — 1
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