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Huguangyan Maar Lake

Guangdong, Zhanjiang, Huguangyan Maar Lake, China

Other media

Type
Other medium

8 m lateritic profile on basalt beside Huguangyan Maar Lake (Zhanjiang, Guangdong), tropical climate, profile age about 78 ka; kaolinite, goethite, quartz, hematite and ilmenite. Soils are lighter than the basalt: iron oxides retain 121Sb and 123Sb goes to the waters; atmospheric input (rain, litter) dominant in the upper 4 m (Wu et al., 2024). Indicative coordinates (Huguangyan lake). Water of the lake next to the profile (0.111 to 0.117 ng/mL Sb), the heaviest of the study: receives heavy Sb leached from the lateritic soils.

δ123Sb in ‰ (per mil) Values of the same system

Standard : NIST SRM 3102a

ValueRangenMineral or matrixSource
0.379 ± 0.014 ‰0.369 / 0.389 ‰2lake water
Mean and standard deviation recalculated from 2 analyses, +0.369 to +0.389 (ZJ-LA1 +0.389; ZJ-LA2 +0.369); published as ε123Sb, ± 0.028 ‰ (2 SD) each.
Wu et al. (2024), Antimony isotopic fractionation during intensive chemical weathering of…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Huguangyan Maar Lake, isotope signatures. https://www.isofind.tech/isotopes/en/sites/lac-de-maar-de-huguangyan/ (accessed 2026-10-16).

@misc{isofind2026huguangyanmaarlakeisotopesign,
  title = {Huguangyan Maar Lake, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/lac-de-maar-de-huguangyan/},
  note = {Accessed 2026-10-16}
}

Updated : 2026-10-16