Beryozovsky coal (Kansk-Achinsk Basin)
Krasnoyarsk Krai, Kansk-Achinsk Basin, Russia
Othercharbon (Hg)
- Type
- Coal deposit (coal of unspecified rank, Jurassic)
Coal seam of unspecified rank, of Jurassic age; mercury with a mean δ202Hg of -0.50 ‰ and Δ201Hg of -0.53 ‰ (Biswas et al., 2008). Non-homogenised sample (VTI); most negative Δ201Hg of the coals studied. Indicative coordinates (Berezovsky 1 mine at Sharypovo, after Global Energy Monitor).
δ202Hg in ‰ (per mil) Values of the same system
Standard : NIST SRM 3133
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −0.5 ± 0.46 ‰ | −1 / −0.11 ‰ | 3 | coal (coal of unspecified rank) Mean and standard deviation recalculated from 3 subsamples, the standard deviation reflects deposit heterogeneity; subsamples combusted separately: -0.11 ± 0.04 ‰ (2SD 2 analyses); -0.39 ± 0.01 ‰ (2SD 2 analyses); -1.00 ± 0.04 ‰ (2SD 3 analyses); 7 analyses in total; non-homogenised sample (VTI); most negative Δ201Hg of the coals studied. | Biswas et al. (2008), Natural mercury isotope variation in coal deposits and organic soil… |
Δ201Hg in ‰ (per mil) Values of the same system
Standard : NIST SRM 3133
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −0.53 ± 0.03 ‰ | −0.56 / −0.51 ‰ | 3 | coal (coal of unspecified rank) Mean and standard deviation recalculated from 3 subsamples, the standard deviation reflects deposit heterogeneity; subsamples combusted separately: -0.56 ± 0.07 ‰ (2SD 2 analyses); -0.53 ± 0.08 ‰ (2SD 2 analyses); -0.51 ± 0.05 ‰ (2SD 3 analyses); 7 analyses in total; non-homogenised sample (VTI); most negative Δ201Hg of the coals studied. | Biswas et al. (2008), Natural mercury isotope variation in coal deposits and organic soil… |
Δ199Hg in ‰ (per mil) Values of the same system
Standard : NIST SRM 3133
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −0.63 ± 0.03 ‰ | −0.66 / −0.61 ‰ | 3 | coal (coal of unspecified rank) Mean and standard deviation recalculated from 3 subsamples, the standard deviation reflects deposit heterogeneity; subsamples combusted separately: -0.66 ± 0.06 ‰ (2SD 2 analyses); -0.63 ± 0.10 ‰ (2SD 2 analyses); -0.61 ± 0.01 ‰ (2SD 3 analyses); 7 analyses in total; non-homogenised sample (VTI); most negative Δ201Hg of the coals studied. | Biswas et al. (2008), Natural mercury isotope variation in coal deposits and organic soil… |
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- Huoshaoyun China
- Zankan China
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Cite this page
IsoFind Atlas (2026). Beryozovsky coal (Kansk-Achinsk Basin), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/charbon-de-berezovsky-bassin-de-kansk-atchinsk/ (accessed 2026-10-15).
@misc{isofind2026beryozovskycoalkanskachinskba,
title = {Beryozovsky coal (Kansk-Achinsk Basin), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/charbon-de-berezovsky-bassin-de-kansk-atchinsk/},
note = {Accessed 2026-10-15}
}Updated : 2026-10-15