Logo image
Geochemistry of Se and Te in arsenian pyrite; new evidence for the role of Se and Te hydrothermal complexes in carlin and epithermal-type deposits
Conference proceeding   Open access   Peer reviewed

Geochemistry of Se and Te in arsenian pyrite; new evidence for the role of Se and Te hydrothermal complexes in carlin and epithermal-type deposits

Stephen E. Kesler, Artur P. Deditius and Stephen Chryssoulis
Opas - Geologian Tutkimuskeskus, Vol.53, pp.57-59
Field workshop of IGCP 486, Workshop (Espoo, Finland, 26/08/2007–31/08/2007)
2007
url
https://tupa.gtk.fi/julkaisu/opas/op_053.pdfView
Published (Version of Record) Open

Abstract

arsenic carlin-type deposits Economic geology, geology of ore deposits epithermal processes geochemical controls geochemistry Geochemistry of rocks, soils, and sediments gold gold ores hydrothermal conditions IGCP metal ores metals mineral deposits, genesis ore-forming fluids pyrite selenium silver sulfides tellurium trace elements
Analyses by electron microprobe and secondary-ion mass spectrometry provide information on the relation of Se and Te to other trace elements in arsenian pyrite from Carlin-type and low-sulfidation type epithermal deposits. Correlations between abundances of Se and Te and the other trace elements probably reflect similar behavior in hydrothermal solution and possibly the presence of as yet unknown complexes. Strongest correlations are seen between Te and both Au and Ag in Carlintype deposits and between Te and Ag in epithermal-type deposits; correlations of Au and Ag with Se are uniformly poor. Although correlations with Te are strong, crossplots indicate low Te:Au and Te:Ag ratios of ~0.1 or less, suggesting that Te was not sufficiently abundant to complex either Au or Ag. These results suggest that Se complexes are not present and that Te complexes, though present, are of secondary importance as an agent of metal transport.

Details

Metrics

65 Record Views
Logo image