· Such gold enrichment in low-temperature Si–Ba-rich ores resembles gold deposition in the uppermost chert–barite-rich cap in ancient VMS hydrothermal systems on land (Huston …
view moreThe supergene enrichment of gold in deposits may take place by a simple mechanical process, by chemical means, or by a combination of these. First, the enrichment may be primarily the result of the chemical removal of a large part …
view more· Therefore, a notable enrichment in gold in moderately evolved lavas (Mg# = 50 ± 5) without corresponding increase of copper cannot result from melt evolution. This decoupling …
view more· We show that the influence of the Iceland plume on the Mid-Atlantic Ridge progressively enriches the oceanic crust in Au along the Reykjanes Ridge by as much as 13 …
view more· FENG YueChuan, QIU KunFeng, WANG DaZhao, SHA WuJin, LI Shuang. 2022. Forming conditions of tellurides and their constraints on gold enrichment in Linglong gold …
view more· Previously unobserved chains of gold nanoparticles occur at the boundary of early sphalerite and chalcopyrite, distinct from gold observed in massive sphalerite as identified in …
view more· The gold mineralization in the Xiaotongjiapuzi gold deposit was the result of magmatic-hydrothermal processes. We propose two key factors: i) abundant defects in non-stoichiometric Fe-sulfides, and ii) replacement processes can cause invisible gold enrichment in Fe-sulfides in the Liaodong Peninsula.
view more· We present a simple method by which gold nanoparticles (AuNPs) are used to simultaneously isolate and enrich for free or modified thiol-containing peptides, thus facilitating the identification of protein S-modification sites. Here, protein disulfide isomerase (PDI) and dual specificity phosphatase 12 (DUSP12 or hYVH1) were S-nitrosylated or S-glutathionylated, …
view more· Similar enrichment behavior for other metals implies that no gold-enriched precursor melt is required and fractional crystallization can enrich the Au concentration to economic levels. The low content of accessory oxides and sulfides, the absence of early Cl-bearing fluids, the volatile content in the melt, and a prolonged crystallization ...
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view more· These tellurides are the first gold-bearing phase to be identified in these chimneys, and the Bi-Au association suggests that gold enrichment up to 91 ppm is due to scavenging by liquid bismuth.
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view more· For gold, the necessary enrichment factor is extreme and approaching 10,000 so there is a challenge as to how enough gold can be accumulated to form a deposit. There is approximately 6 t of gold at background levels in a cubic kilometre of average rock. This background gold is evenly dispersed at the nanometric-scale.
view more· In order to study the mechanism of gold enrichment, 18 samples collected around deep faults were analyzed by geochemical methods. The results indicate that the gold accumulation in Jiyang Depression is closely related to the mantle fluids and sulfur polycyclic aromatic hydrocarbon (S-PAH) in oil and source rocks.
view more· The origins of high-grade hydrothermal ore deposits are debated, but active geothermal systems provide important clues to their formation 1,2.The highest concentrations …
view more· High gold contents (to 10.1 ppm, avg 1.4 ppm, n = 34) occur in pyrrhotite-rich massive sulfide samples from the sediment-covered floor of the Escanaba trough, the slow-spreading, southernmost segment of Gorda Ridge. These concentrations reflect the presence of primary gold, formed during high-temperature hydrothermal activity in mounds and chimneys, and …
view more· The difference of gold enriching ability of bacteria and algae in different environment is studied, and the mechanism of gold enrichment of organisms is discussed. 、、、、 ,, ...
view more· High gold contents (to 10.1 ppm, avg 1.4 ppm, n = 34) occur in pyrrhotite-rich massive sulfide samples from the sediment-covered floor of the Escanaba trough, the slow-spreading, southernmost segment of Gorda Ridge. These concentrations reflect the presence of primary gold, formed during high-temperature hydrothermal activity in mounds and chimneys, and …
view more· On the other hand, the residual gold enrichment, under supergene conditions, can be formed by Ag dissolution from Au ± Ag hypogene particles (Bowell, 1992). Pyrite is a …
view more· High gold contents (to 10.1 ppm, avg 1.4 ppm, n = 34) occur in pyrrhotite-rich massive sulfide samples from the sediment-covered floor of the Escanaba trough, the slow-spreading, …
view more· The difference of gold enriching ability of bacteria and algae in different environment is studied, and the mechanism of gold enrichment of organisms is discussed. …
view more· Gold was mobilized from earlier formed primary gold minerals and transported as aqueous chloride complexes. The reduction of Au(III) by residual Fe2+ in partly altered pyrrhotite and adsorption of colloids by Fe oxyhydroxides may have influenced the location of secondary gold grains within the alteration front.
view more· Gold Enrichment and the Bi-Au Association in Pyrrhotite-Rich Massive Sulfide Deposits, Escanaba Trough, Southern Gorda Ridge September 2005 Economic Geology 100(6):1135-1150
view more· Download Citation | Gold Enrichment and the Bi-Au Association in Pyrrhotite-Rich Massive Sulfide Deposits, Escanaba Trough, Southern Gorda Ridge | High gold contents (to 10.1 ppm, avg 1.4 ppm, n ...
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view moreThe supergene enrichment of gold in deposits may take place by a simple mechanical process, by chemical means, or by a combination of these. First, the enrichment may be primarily the result of the chemical removal of a large part of the gangue minerals, in which case the gold migrates slowly downward by gravity or is left behind as a residual component. Such enrichments …
view more· The native gold grains from the basalts may have been inherited by the younger (ca. 140 Ma) Carlin-type ores in the Youjiang basin, which are indicative of gold pre-enrichment in the basin.
view more· Gold enrichment in hydrothermal sulfides from the Okinawa Trough: An in situ LA-ICP-MS Ore Geology Reviews ( IF 3.809) Pub Date :, DOI: 10.1016/j.oregeorev.2019.103255 Yaoyao Zhang, Fengyou Chu, Zhenggang Li, Yanhui Dong, Hao Wang, Xiaohu Li, Jiangping Long
view more· We show that the influence of the Iceland plume on the Mid-Atlantic Ridge progressively enriches the oceanic crust in Au along the Reykjanes Ridge by as much as 13 times normal levels, over a distance of ∼600 km, and that the enrichment can be attributed to specific plume components.
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