Using a sample from a terrestrial hot spring (pH 6.8, 60 °C), we enriched a thermophilic microbial consortium performing anaerobic autotrophic oxidation of hydrothermal …
WhatsApp: +86 18221755073Here, we report greenalite and fluorapatite (FAP) nanoparticles in the oldest, well-preserved jaspilites from the ~3.5-billion-year Dresser Formation, Pilbara Craton, Australia. We argue that both phases are vent plume particles, …
WhatsApp: +86 18221755073In two sphaerosiderite horizons, sphaerosiderites contain pyrite inclusions with diameters >20 µm, and the pyrite inclusions themselves contain siderite inclusions.
WhatsApp: +86 18221755073In two sphaerosiderite horizons, sphaerosiderites contain pyrite inclusions with diameters >20 µm, and the pyrite inclusions themselves contain siderite inclusions.
WhatsApp: +86 18221755073Here, we report greenalite and fluorapatite (FAP) nanoparticles in the oldest, well-preserved jaspilites from the ~3.5-billion-year Dresser Formation, Pilbara Craton, Australia. We argue that both phases are vent plume particles, whereas coexisting hematite is linked to secondary oxidation.
WhatsApp: +86 18221755073The partitioning of As and Au into pyrite was studied by replacing siderite (FeCO 3) by pyrite (FeS 2) by reacting the Fe carbonate with H 2 S-containing aqueous fluids under experimental conditions similar to those of CTGD formation (i.e., 200°C, fluid-dominated conditions, 0.05 m H 2 S, and
WhatsApp: +86 18221755073Pyrite is consistently found at the outermost parts of the replaced siderite grains, while some siderite grains also display full replacement by pyrite (Fig. 1). In experiments with lower concentrations of the acetic acid buffer, the pyrite yield was highest with a mean phase content of 45 wt %.
WhatsApp: +86 18221755073Using a sample from a terrestrial hot spring (pH 6.8, 60 °C), we enriched a thermophilic microbial consortium performing anaerobic autotrophic oxidation of hydrothermal siderite (FeCO 3), with CO...
WhatsApp: +86 18221755073Arsenian pyrite is the major host mineral of gold in Carlin type gold deposit (CTGD) and forms during the interaction of H2S bearing hydrothermal fluids with Fe-bearing carbonates (e.g.,...
WhatsApp: +86 18221755073The most common iron carbonate is siderite (FeCO 3), a frequent constituent of carbonate sediments and rocks on Earth. Siderite has a low-temperature transition at 30–35 K (Housen et al., 1996), distinctively different from that of pyrrhotite (Section 5.08.3.9). Siderite is …
WhatsApp: +86 18221755073The most common iron carbonate is siderite (FeCO 3), a frequent constituent of carbonate sediments and rocks on Earth. Siderite has a low-temperature transition at 30–35 K (Housen et al., 1996), distinctively different from that of pyrrhotite (Section 5.08.3.9). Siderite is paramagnetic at ordinary temperatures and carries no NRM.
WhatsApp: +86 18221755073The lack of pyrite and the presence of disseminated siderite in the incubated sediment suggest the heterogeneity of localized geochemistry within the sediment. This could partly explain the occurrence of siderite concretion only in certain microenvironment of the marsh.
WhatsApp: +86 18221755073Arsenian pyrite is the major host mineral of gold in Carlin type gold deposit (CTGD) and forms during the interaction of H2S bearing hydrothermal fluids with Fe-bearing carbonates (e.g.,...
WhatsApp: +86 18221755073Pyrite is consistently found at the outermost parts of the replaced siderite grains, while some siderite grains also display full replacement by pyrite (Fig. 1). In experiments with …
WhatsApp: +86 18221755073Our proposed numerical models yield results that closely align with the oscillatory zoning patterns observed in pyrite-siderite from the Xinqiao massive sulfide deposit in Central China.
WhatsApp: +86 18221755073The partitioning of As and Au into pyrite was studied by replacing siderite (FeCO 3) by pyrite (FeS 2) by reacting the Fe carbonate with H 2 S-containing aqueous fluids under experimental conditions similar to those of …
WhatsApp: +86 18221755073Fluid mediated replacement of siderite by pyrite is a fast and effective process to transform Fe-bearing carbonates into sulfides that works via a coupled dissolution …
WhatsApp: +86 18221755073The lack of pyrite and the presence of disseminated siderite in the incubated sediment suggest the heterogeneity of localized geochemistry within the sediment. This could partly explain the occurrence of siderite concretion …
WhatsApp: +86 18221755073Our proposed numerical models yield results that closely align with the oscillatory zoning patterns observed in pyrite-siderite from the Xinqiao massive sulfide deposit in Central China.
WhatsApp: +86 18221755073Fluid mediated replacement of siderite by pyrite is a fast and effective process to transform Fe-bearing carbonates into sulfides that works via a coupled dissolution-reprecipitation reaction.
WhatsApp: +86 18221755073