Talatui

Transbaikalia, Darasun gold district, Russia

Other hydrothermalAu

Type: Gold zones and lenses with magnetite and sulphides

Darasun district: gold veins controlled by fractures related to the collision of the Siberian and Sino-Korean continents, associated with Jurassic to Cretaceous intrusions of the Amudzhikan-Sretensky Complex, without later metamorphic overprint; host Palaeozoic metagabbros (Kruchininsky Complex) and granitoids. 7 km northwest of Teremkyn: mineralized zones and lenses related to dykes, in metagabbros with propylitic and potassic alteration; average 8.5 g/t Au. Baksheev et al. (2015): fluid from -2.5 to +2.2 ‰ near 400 °C, boron from the metagabbros.

δ11B in ‰ (per mil) Values of the same system

Standard : NIST SRM 951

Value	Range	n	Mineral or matrix	Source
	−5.2 / −0.9 ‰	9	isolated vein tourmaline (Ca-rich oxy-dravite), sample 154/05 Published range and standard deviation (1.5 ‰), no mean. No significant core-rim difference.	Baksheev et al. (2015), Geochemical evolution of tourmaline in the Darasun gold district,…

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Cite this page

IsoFind Atlas (2026). Talatui, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/talatui/ (accessed 2026-10-20).

@misc{isofind2026talatuiisotopesignatures,
  title = {Talatui, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/talatui/},
  note = {Accessed 2026-10-20}
}

Updated : 2026-10-20