Research Article
Geochemistry, Paragenesis, and Wall-Rock Alteration of the Qatruyeh Iron Deposits, Southwest of Iran: Implications for a Hydrothermal-Metasomatic Genetic Model
Figure 4
(a) Panorama photograph of the Chah Anjir intrusive unit, chilled margin and calcareous sandstone, and shale unit with Dictyoconous sp. fossil, (b) comparison between fresh and altered dolomitic marble.
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