Dangping
Xihuashan ore field, Dayu County, Ganzhou, Jiangxi, China
Other hydrothermalW
- Type
- Wolframite-quartz veins
Wolframite-quartz vein deposit in a Yanshanian granite. According to Zhang (1988), wolframite at about +5 ‰ and quartz at about +12 ‰, formed at about 300 to 350 °C from re-equilibrated magmatic water of W-Sn granites. Mindat coordinates (to the minute). Indicative coordinates.
δ18O in ‰ (per mil) Values of the same system
Standard : V-SMOW
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 11.95 ± 0.63 ‰ | 2 | quartz of wolframite-beryl-quartz veins Published mean and standard deviation from 2 samples, Table 1; individual values not given. | Zhang (1988), Oxygen isotope studies of wolframite in tungsten ore deposits of south Chin… | |
| 5.1 ± 0.14 ‰ | 2 | wolframite of wolframite-beryl-quartz veins Published mean and standard deviation from 2 samples, Table 1; individual values not given. | Zhang (1988), Oxygen isotope studies of wolframite in tungsten ore deposits of south Chin… |
Deposits of the same type
- Xihuashan China
- Piaotang China
- Maoping (tungsten, Jiangxi) China
- Yaoling China
- Dajishan China
- Kuimeishan (Guimeishan) China
- Yaogangxian China
- Hongling China
Cite this page
IsoFind Atlas (2026). Dangping, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/dangping/ (accessed 2026-10-13).
@misc{isofind2026dangpingisotopesignatures,
title = {Dangping, isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/dangping/},
note = {Accessed 2026-10-13}
}Updated : 2026-10-13