Get Essential, free

Delyuvial'noe (Delyuvial'nyi)

Sakha (Yakutia), Adychanskii ore region (Adycha-Taryn zone), Russia

Orogenic goldAu

Type
Impregnation-vein gold in sedimentary rocks (metasomatic)

Adychanskii gold region, in the northern Verkhoyansk-Kolyma gold province: Upper Triassic argillites and siltstones sliced by thrusts, Early Cretaceous S-type granitoids; Delyuvial'noe, Lazovskoe and Sentachan ore fields. Aristov et al. (2017): two fluids of similar temperature and salinity, generated by metagenesis and mobilised during collision (quartz-A at 290-340 °C and 1550 bar, near 6 km; quartz-B, -AB and -C at 250-380 °C and 350-1250 bar, from 3.5 to 1.5 km). Impregnation-vein occurrence of the Delyuvial'noe field (167 t Au at 2 ppm according to OAO Yangeologiya, 2005-2008), grey fine-grained quartz (quartz-B) without carbonate or stibnite formed by metasomatic replacement; fluid at 280-380 °C, 6.5 ± 1 wt% NaCl equiv. and 830-930 bar, N2 and CH4 dominant. Galena R-30: δ34S +2.0 ‰, 206Pb/204Pb 18.245, model age 120 Ma. Coordinates not published (schematic map only, frame 136°40'-137°20' E, 66°20'-66°40' N).

δ34S in ‰ (per mil) Values of the same system

Standard : V-CDT

ValueRangenMineral or matrixSource
2 ‰1galena
Single analysis (R-30). Fluid H2S estimated at +4.0 ‰ at 300 °C (isotope thermometry and inclusions).
Aristov et al. (2017), Sources of fluids and material for gold and antimony mineralizatio…

206Pb/204Pb isotope ratio, no unit Values of the same system

Standard : Non précisé dans la publication

ValueRangenMineral or matrixSource
18.2451galena
Single analysis (R-30). Model age of 120 Ma (model U/Pb and Th/U in Table 1). The points plot on a secondary isochron of slope 0.158 (lead source near 2380-2350 Ma).
Aristov et al. (2017), Sources of fluids and material for gold and antimony mineralizatio…

207Pb/204Pb isotope ratio, no unit Values of the same system

Standard : Non précisé dans la publication

ValueRangenMineral or matrixSource
15.5211galena
Single analysis (R-30). Model age of 120 Ma (model U/Pb and Th/U in Table 1). The points plot on a secondary isochron of slope 0.158 (lead source near 2380-2350 Ma).
Aristov et al. (2017), Sources of fluids and material for gold and antimony mineralizatio…

208Pb/204Pb isotope ratio, no unit Values of the same system

Standard : Non précisé dans la publication

ValueRangenMineral or matrixSource
38.1521galena
Single analysis (R-30). Model age of 120 Ma (model U/Pb and Th/U in Table 1). The points plot on a secondary isochron of slope 0.158 (lead source near 2380-2350 Ma).
Aristov et al. (2017), Sources of fluids and material for gold and antimony mineralizatio…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Delyuvial'noe (Delyuvial'nyi), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/delyuvial-noe-delyuvial-nyi/ (accessed 2026-10-19).

@misc{isofind2026delyuvialnoedelyuvialnyiisoto,
  title = {Delyuvial'noe (Delyuvial'nyi), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/delyuvial-noe-delyuvial-nyi/},
  note = {Accessed 2026-10-19}
}

Updated : 2026-10-19