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Mariinsky (Malyshevo)

Central Urals, Ural emerald belt (Malyshevo, Sverdlovsk Oblast), Russia

OtherBe (émeraude)

Type
Emerald, alexandrite and phenakite in phlogopite schists (schist-hosted type)

Largest emerald, alexandrite and phenakite deposit of the Ural emerald belt, 80 km NE of Yekaterinburg, in a serpentinite melange zone between the Adui and Malyshevo plutons; lenticular emerald-bearing phlogopite schist bodies (type 1 veins) cut by late emerald-free pockets and veinlets (type 2). Baksheev et al. (2018): tourmalines from -11.3 to -8.4 ‰ (mean -10.1 ‰), formed at about 420 to 360 °C; fluid from -8.6 to -5.7 ‰, mixed boron from granites and ultramafic host rocks. Indicative coordinates of Malyshevo, not published in the article.

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

Standard : NIST SRM 951

ValueRangenMineral or matrixSource
−10.4 ± 0.6 ‰−10.9 / −9.3 ‰9tourmaline of emerald-bearing phlogopite veins (types 1a to 1c)
Mean and standard deviation recalculated from 9 analyses, -10.9 to -9.3 (M-8 -10.4; M-8 -10.4; M-102 -9.6; M-102 -9.3; M-104 -10.6; M-104 -10.5; KA-5 -10.8; KA-5 -10.8; KA-5 -10.9). Phlogopite-tourmaline veins, with talc, tremolite or plagioclase depending on the sample; formed at about 410 to 420 °C (tourmaline-biotite thermometer).
Baksheev et al. (2018), Chemical and boron isotopic composition of tourmaline from the Ma…
−10.1 ± 0.8 ‰11tourmaline of chromite-phlogopite-paragonite alteration (type 1d, BAK-1)
Published mean and standard deviation of 11 analyses.
Baksheev et al. (2018), Chemical and boron isotopic composition of tourmaline from the Ma…
−10 ± 0.8 ‰−11.1 / −8.9 ‰14tourmaline of late emerald-free pockets, veinlets and lenses (type 2)
Mean and standard deviation recalculated from 14 analyses, -11.1 to -8.9 (Chb -10.0; Chb -10.0; M-127 -11.0; M-127 -10.5; M-112 -10.8; M-112 -10.5; M-115 -11.1; M-115 -10.8; M-131 -9.8; M-131 -9.7; M-134 -9.1; M-134 -8.9; M-119 -8.9; M-119 -8.9). Plagioclase-quartz pockets, fluorite or margarite veinlets, topaz-paragonite lens; margarite veinlets formed at about 350 to 360 °C.
Baksheev et al. (2018), Chemical and boron isotopic composition of tourmaline from the Ma…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Mariinsky (Malyshevo), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/mariinsky-malyshevo/ (accessed 2026-10-19).

@misc{isofind2026mariinskymalyshevoisotopesign,
  title = {Mariinsky (Malyshevo), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/mariinsky-malyshevo/},
  note = {Accessed 2026-10-19}
}

Updated : 2026-10-19