About: The importance of black shales in the origin of the Amantaytau orogenic gold deposit in Uzbekistan: evidence from pyrite chemistry and sulfur isotope data     Goto   Sponge   NotDistinct   Permalink

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  • The local host rock, Late Ordovician – Early Silurian carbonaceous shales, have likely been an important source of Au, As, Ni, and S in the formation of the shear zone-hosted Amantaytau orogenic gold deposit. Syn-depositional pyrite in these shales contain, elevated Au, As, and Ni concentrations of, on average, 0.34, 1658, and 1971 ppm, respectively. The 34S values for pyrite (–0.13 to +7.30 promile CDT) from barren and mineralized samples are consistent with marine sulfate being the principal source of the ore sulfur. Assuming a formation temperature of between 300 and 400 oC for the main stage of mineralization, as indicated by the alteration mineral assemblage, the calculated δ18Ofluid is between 9.5 and 13.4 promile V-SMOW, which points at a metamorphic origin for the ore fluid.
  • The local host rock, Late Ordovician – Early Silurian carbonaceous shales, have likely been an important source of Au, As, Ni, and S in the formation of the shear zone-hosted Amantaytau orogenic gold deposit. Syn-depositional pyrite in these shales contain, elevated Au, As, and Ni concentrations of, on average, 0.34, 1658, and 1971 ppm, respectively. The 34S values for pyrite (–0.13 to +7.30 promile CDT) from barren and mineralized samples are consistent with marine sulfate being the principal source of the ore sulfur. Assuming a formation temperature of between 300 and 400 oC for the main stage of mineralization, as indicated by the alteration mineral assemblage, the calculated δ18Ofluid is between 9.5 and 13.4 promile V-SMOW, which points at a metamorphic origin for the ore fluid. (en)
Title
  • The importance of black shales in the origin of the Amantaytau orogenic gold deposit in Uzbekistan: evidence from pyrite chemistry and sulfur isotope data
  • The importance of black shales in the origin of the Amantaytau orogenic gold deposit in Uzbekistan: evidence from pyrite chemistry and sulfur isotope data (en)
skos:prefLabel
  • The importance of black shales in the origin of the Amantaytau orogenic gold deposit in Uzbekistan: evidence from pyrite chemistry and sulfur isotope data
  • The importance of black shales in the origin of the Amantaytau orogenic gold deposit in Uzbekistan: evidence from pyrite chemistry and sulfur isotope data (en)
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  • RIV/00025798:_____/13:00000098!RIV14-MSM-00025798
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  • 79225
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  • RIV/00025798:_____/13:00000098
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  • Amantaytau, black shale, orogenic gold, sedimentary Au source, sulfur isotopes, pyrite chemistry (en)
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  • [A1E846AFD537]
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  • Uppsala
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  • Uppsala
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  • Mineral deposit research for high-tech world. Proceedings of the 12th Biennial SGA Meeting
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  • Pašava, Jan
  • Vymazalová, Anna
  • Dobeš, Petr
  • Frimmel, Hartwig
  • Jukov, Alexander
  • Koneev, Rustam
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  • Geological Survey of Sweden
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  • 978-91-7403-207-9
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