- journal_title：American Mineralogist
- Contributor：Cristiana L. Ciobanu ; Nigel J. Cook ; Satoshi Utsunomiya ; Masashi Kogagwa ; Leonard Green ; Sarah Gilbert ; Benjamin Wade
- Publisher：Mineralogical Society of America
- Date：2012-
- Format：text/html
- Language：en
- Identifier：10.2138/am.2012.4207
- journal_abbrev：American Mineralogist
- issn：0003-004X
- volume：97
- issue：8-9
- firstpage：1515
- section：Letters
Pyrite, the most abundant sulfide on Earth and a common component of gold deposits, can be a significant host for refractory gold. This is the first documentation of pore-attached, composite Au-telluride nanoparticles in “arsenic-free” pyrite. Trace elements mapping in pyrite from an intrusion-hosted Au deposit with orogenic overprint (Dongping, China) shows trails of tellurides overlapping Co-Ni-zonation. Intragranular microfracturing, anomalous anisotropy, and high porosity are all features consistent with devolatilization attributable to the orogenic event. The pyrite-hosted nanoparticles are likely the “frozen,” solid expression of Te-rich, Au-Ag-Pb-bearing vapors discharged at this stage. Nanoparticle formation, as presented here, provides the “smallest-scale” tool to fingerprint Au-trapping during crustal metamorphism