The distributions of trace elements in pyrite were studied samples high-grade gold ores from the Talatui, Teremkyn, and Darasun deposits. paper presents LA-ICP-MS data on concentrations mineral deposits goldfield, which produced by a single fluid–magmatic system at various temperatures. high-temperature was found to be enriched Co, Se, W, whereas medium-temperature Cu, Zn, Ag, Te, As, In. behav...

The Mount Milligan deposit, centred at latitude SS”O8’ north and longitude 124”04’ west, is 100 kilometres westsouthwest of Mackenzie and 160 kilometres northwest of Prince George in central British Columbia. The deposit occurs in gently rolling topography (Plate 2-6-l) 5 kilometres due south of Mount Milligan. Access to the property is by a 93.kilometre logging road that connects with the Hart...

Stikine Terrane arc rocks in the re,:ion host !;(m:ral copper-gold and copper-molybdenum ocnlwerlces (MINFILE 104 G and H). The volcrrnic strat.i,:raphy hosting these deposits is, however, poorly const:aimd. The Tatogga Lake project will attemp; to characterize individual deposits, desclibe their h a 1 and rcgictnal stratigraphic and structural settings, and deternme the ages of magmatism ...

Over the years, many geological exploration reports and considerable data have been accumulated during prospecting of Jiapigou gold metallogenic belt (JGMB). It is very important to fully utilize these mineralogical big guide future exploration. This work collects original textual different deposits in JGMB constructs a knowledge graph (KG) for based on deep learning (DL) natural language proce...

Previous secondary ion mass spectr.ometry (SIMS) studies of extended impact features from LDEF capture cell experiment AO187-2 showed that it is possible to distinguish natural and manmade particle impacts based on the chemical composition of projectile residues. The same measurement technique has now been applied to specially prepared gold target impacts from experiment AO187-1 in order to ide...

The known dimensions of hydrothermal fluid circulation associated with emplacement of the 2.055-Ga Bushveld Igneous Complex (BIC) are extended with new isotopic ages for Paleoproterozoic mineral deposits in wallrocks (Transvaal Supergroup) surrounding the BIC. A fluorite-rich Mississippi Valley–type (MVT) deposit in the Zeerust district, dated at 2.05 Ga (Sm-Nd isochron age), has Nd isotopic co...