Exploring the interplay of under-deposit corrosion and microbiologically influenced corrosion in the presence of deposits with varied electrical conductivities. [PDF]
Diaz-Mateus MA +5 more
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Mobilization of isotopically heavy sulfur during serpentinite subduction. [PDF]
Schwarzenbach EM +8 more
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Magmatic-hydrothermal fluid evolution of the tin-polymetallic metallogenic systems from the Weilasituo ore district, Northeast China. [PDF]
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Metal(loid)s and their bioaccessibility in urban soils from residential areas of a medieval mining town. [PDF]
Ettler V +5 more
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Abiotic synthesis during the interaction of ferrous chloride-rich silicic fluids with marble under high-grade metamorphic conditions. [PDF]
Fei C, Guo S, Li Y, Liu J.
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Low-Temperature Aqueous Alteration of Chondrites. [PDF]
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Mantle oxidation by sulfur drives the formation of giant gold deposits in subduction zones. [PDF]
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Ore Genesis of the Jiawula Pb-Zn-Ag Deposit, Inner Mongolia: Constraints from C-H-O Isotopes, In Situ S Isotopes, Fluid Inclusions, and LA-ICP-MS Analysis of Chalcopyrite. [PDF]
Li H, Mi W, Zuo Y, Xu J, Ren Z.
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A review on pyrrhotite oxidation
Journal of Geochemical Exploration, 2004The non-stoichiometric compounds of iron sulphide named pyrrhotite (Fe1−xS) are often associated with pyrite (FeS2) in sulphidic ores and their waste products. The factors affecting pyrite and pyrrhotite oxidation are similar but the latter has received much less attention.
Nelson Belzile
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Pyrrhotite phases and pyrrhotite-pyrite relationships; Renison Bell, Tasmania
Economic Geology, 1970Hexagonal and monoclinic pyrrhotite, pyrite as isolated cubes within massive pyrrhotite or in massive form cut by pyrrhotite, paragenesis, mineragraphy, x-ray diffraction ...
Simon John Haynes, Patrick Arthur Hill
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