Filamentary native gold from the Elatsite porphyry Cu-Au deposit ...
Filamentary native gold from the Elatsite porphyry Cu-Au deposit ...
Filamentary native gold from the Elatsite porphyry Cu-Au deposit ...
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<strong>Filamentary</strong> <strong>native</strong> <strong>gold</strong> <strong>from</strong><strong>the</strong> <strong>Elatsite</strong> <strong>porphyry</strong> <strong>Cu</strong>-<strong>Au</strong><strong>deposit</strong>, Srednogorie zone,Bulgaria
<strong>Au</strong>-Ag-Te-Se <strong>deposit</strong>sIGCP Project 486, 2005 Field Workshop, Kiten, Bulgaria, 14-19 SeptemberIvan K. Bonev, Rumen Petrunov, Radostina AtanassovaGeological InstituteBulgarian Academy of Sciences1113 Sofia, Bulgaria;E-mail: bonev@geology.bas.bg
Native <strong>gold</strong> is known in highly variable morphology- As octahedral, cubic, dodecahedral and more complex crystals- In skeletal and dendritic forms- As irregular grains- As prismatic elongated or platy grains- Rarely, as hair-like and fine fibrous formationsPetrovskaya (1973) assigned <strong>the</strong>m to a morphogenetic type of notwellbounded and rounded crystals
Bundles of <strong>gold</strong>filaments in a smallcavity of magnetitebornite-chalcopyriteore
A group of filamentsAn enlargeddetail
10 µmThe twin-peakedtermination of one of <strong>the</strong>filaments:cubic-octahedral habit
Single crystal filament with changeable growth direction andstepped lateral faces
10 µmA bundle of fibers in twinned positions, bounded by cubic faces;1 and 2: twinned along (111) crystals in two orientations
A fibre with longitudinal (111) twinplane
10 µmSurface morphology :complex vicinals on o(111)10 µm
cDifferent tips of <strong>gold</strong>filaments: a) moreindividualised distortedcrystal termination; b) and c)splitted terminations withcomplex shapes (triple in b,and double in c).Crystal forms: d{110}, o{111}, a{100}, m{311}, f{310}. Scale bars - 10 µm
Gold filaments withchangeablethickness
Complex steppedsurfaces of somefilaments10 µm
A bundle of mechanically distorted subparallel filaments(A detail on right: translation gliding)
The <strong>Elatsite</strong><strong>deposit</strong>Chemical composition of filamentary <strong>gold</strong> and compositional fields of<strong>gold</strong> <strong>from</strong> <strong>the</strong> main ore assemblages: mt-bn-cp, q-cp-py + q-py and q-ga-sph (after data of Kehayov and Bogdanov, 2005, and o<strong>the</strong>rs). Inparticular, mt-bn-cp-II concerns to visible <strong>gold</strong> cutting early bornite
System <strong>Au</strong>-<strong>Cu</strong>-Fe-S<strong>Au</strong> in <strong>Cu</strong> sulphides<strong>Au</strong> transport:Simon, Kesler, Essene, 2000 Gammon & Williams-Jones, 1997Stefansson & Seward, 2003, 2004bornitechalcopyrite600 o C 4,875 ppm 104-125 ppm <strong>Au</strong>Cl 2-400 o C 13-80 ppm 2-4 ppm sulphide complexes
10 µm<strong>Filamentary</strong> crystals ofdifferent thickness.The Chelopech <strong>deposit</strong>
Galena filaments andstraight whiskersMadan ore district
Conclusions- The rare in nature filamentary <strong>gold</strong> in <strong>Elatsite</strong> occurs in small cavities of <strong>the</strong>early magnetite-bornite-chalcopyrite-The filamentary <strong>native</strong> <strong>gold</strong> in <strong>Elatsite</strong> forms not straight crystals boundedby small alternating faces of <strong>the</strong> main crystal forms: a, o, d, f, m- The chemical composition of <strong>the</strong> filamentary <strong>gold</strong> is comparable with this of<strong>the</strong> main chalcopyrite-pyrite stage- Most probably, <strong>the</strong> high-temperature (600-530 o C) <strong>Au</strong>-rich bornite ss is earlycollector for <strong>gold</strong>, by cooling of which (~400 o C) <strong>gold</strong> is separated and re<strong>deposit</strong>edin <strong>the</strong> close vicinity- The extremely non-equilibrium filamentary crystals of <strong>gold</strong> were <strong>deposit</strong>ed<strong>from</strong> highly supersaturated heterogeneous boiling solutions of high salinity