Abstract
Although As-rich, hydrothermal overgrowths on pyrite have been recognized as the primary host phase for Au in Carlin-type deposits in Nevada, the chemical and structural state of the Au has remained unresolved. Spectroscopic and electron imaging techniques have suggested that Au is either structurally bound (e.g., Au1+) or occurs as particles of native Au (Au0), but the latter has never been observed directly. We have determined that Au is present in significant quantities as discrete nanoparticles of native Au (~5.10 nm) in As-rich overgrowths on pyrite from the Screamer deposit in the Carlin trend, Nevada, using analytical and high-resolution TEM and high-angle annular dark-field (HAADF) imaging in STEM mode. Electron microprobe and secondary ion mass spectrometry (SIMS) analyses of the As-rich rims containing the Au-particles reveal that these rims (1.20 µm) contain up to 0.8 wt% Au, among the highest Au-contents ever reported for arsenian pyrite. These observations suggest two possible mechanisms for nanoparticle formation: that Au exceeded its solubility limit in arsenian pyrite causing it to be deposited as nanoparticles of native metal; or that exsolution of native metal from metastable arsenian pyrite was caused by a later event in the history of the deposit.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- The origin of the color of pearls in iridescence from nano-composite structures of the nacre
- “Invisible„ gold revealed: Direct imaging of gold nanoparticles in a Carlin-type deposit
- Behavior of cation vacancy in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites
- Displacement and strain fields around a [100] dislocation in olivine measured to sub-angstrom accuracy
- Kiglapait mineralogy IV: The augite series
- Metasomatic formation of kosmochlor-bearing diopside in peridotite xenoliths from North Island, New Zealand
- Determination of standard thermodynamic properties of sulfides in the Ag-Au-S system by means of a solid-state galvanic cell
- Hydroxyl ordering in igneous apatite
- Accommodation of the carbonate ion in apatite: An FTIR and X-ray structure study of crystals synthesized at 2–4 GPa
- Mg/Si ratios of aqueous fluids coexisting with forsterite and enstatite based on the phase relations in the Mg2SiO4-SiO2-H2O system
- The activity of silica, water, and the equilibration of intermediate and silicic magmas
- The CO2–H2O system: IV. Empirical, isothermal equations for representing vapor-liquid equilibria at 110–350 °C, P ≤ 150 MPa
- Repercussions of size heterogeneity on the measurement of specific surface areas of colloidal minerals: Combination of macroscopic and microscopic analyses
- The crystal-structure of synthetic NaNa2Mg5Si8O21(OH)3, a triclinic C1̄ amphibole with a triple-cell and excess hydrogen
- High-pressure phase transitions in Ca0.2Sr0.8Al2Si2O8feldspar
- Phase transition of Ca-perovskite and stability of Al-bearing Mg-perovskite in the lower mantle
- Mineralogy and petrology of a mullite-bearing pseudotachylyte: Constraints on the temperature of coseismic frictional fusion
- New developments in two-feldspar thermometry
- Ordered distribution of Au and Ag in the crystal structure of muthmannite, AuAgTe2, a rare telluride from Sacarîmb, western Romania
- Polytypism of cookeite in low-grade metapelites of the Cameros Basin, Spain: Lack of correlation of well-ordered polytypes with pressure
- Evolution of mineral compositions during eclogitization of subducting basaltic crust
- Mass balance during retrogression of eclogite-facies minerals in the Rongcheng eclogite, eastern Sulu ultrahigh-pressure terrane, China
- Synthesis of REE and Y phosphates by Pb-free flux methods and their utilization as standards for electron microprobe analysis and in design of monazite chemical U-Th-Pb dating protocol
- The chemistry and crystal structure of okanoganite-(Y) and comparison with vicanite-(Ce)
- An automated system for phase identification and quantitative composition determination using the electron microprobe: Theory and applications
- Piston-cylinder calibration at 400 to 500 MPa: A comparison of using water solubility in albite melt and NaCl melting
- Letter. Comparative planetary mineralogy: V/(Cr + Al) systematics in chromite as an indicator of relative oxygen fugacity
- Letter. Porous titanosilicate nanorods in the structure of yuksporite, (Sr,Ba)2K4(Ca,Na)14(⃞,Mn,Fe) {(Ti,Nb)4(O,OH)4[Si6O17]2[Si2O7]3}(H2O,OH)n, resolved using synchrotron radiation