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Fuwang

Guangdong, south-western rim of the Shanshui Basin (South China Fold Belt), China

Epithermal depositsAg (Pb, Zn)

Type
Silver veins and veinlets in Carboniferous bioclastic limestone (low-sulfidation epithermal)

Adjacent but separate deposits on the south-western rim of the Shanshui Basin, about 75 km south-west of Guangzhou (112°48′01″ to 112°50′13″ E, 23°00′00″ to 23°00′02″ N). Largest silver deposit of the South China Fold Belt (more than 5000 t Ag after Tu, 2000; about 6000 t at 268 g/t in the text), in the Lower Carboniferous Zimenqiao Group limestone, poor in gold. Inclusions at 230 ± 50 °C and 1.6 to 2.6 wt% NaCl equiv.; mixing of magmatic and meteoric water (δD from -59 to -45 ‰, CO2 δ13C from -6.7 to -0.6 ‰, 3He/4He from 0.5930 to 0.8357 Ra, after earlier work). Liang et al. (2007): quartz 40Ar/39Ar plateau age of 64.3 ± 0.1 Ma and fluid-inclusion Rb-Sr isochron of 68 ± 6 Ma (Himalayan orogeny); lead from the Neoproterozoic basement.

206Pb/204Pb isotope ratio, no unit Values of the same system

Standard : NIST SRM 981

ValueRangenMineral or matrixSource
18.848 ± 0.02718.82 / 18.8915galena of the silver ore
Mean and standard deviation recalculated from 5 analyses, 18.820 to 18.891 (CK94 18.820; CK95 18.891; Ck156 18.845; CK157 18.851; CK160 18.834).
Liang et al. (2007), Geology and geochemistry of the adjacent Changkeng gold and Fuwang s…

207Pb/204Pb isotope ratio, no unit Values of the same system

Standard : NIST SRM 981

ValueRangenMineral or matrixSource
15.877 ± 0.0315.848 / 15.9145galena of the silver ore
Mean and standard deviation recalculated from 5 analyses, 15.848 to 15.914 (CK94 15.848; CK95 15.914; Ck156 15.902; CK157 15.873; CK160 15.848).
Liang et al. (2007), Geology and geochemistry of the adjacent Changkeng gold and Fuwang s…

208Pb/204Pb isotope ratio, no unit Values of the same system

Standard : NIST SRM 981

ValueRangenMineral or matrixSource
39.677 ± 0.08639.579 / 39.7864galena of the silver ore
Mean and standard deviation recalculated from 4 analyses, 39.579 to 39.786 (CK94 39.579; CK95 39.786; CK157 39.685; CK160 39.657). Ck156 printed as 36.690, outside the abstract range (39.579 to 39.786) and the other galenas: probable typo, value excluded.
Liang et al. (2007), Geology and geochemistry of the adjacent Changkeng gold and Fuwang s…

87Sr/86Sr isotope ratio, no unit Values of the same system

Standard : Non précisé dans la publication

ValueRangenMineral or matrixSource
0.72015 ± 0.003190.71774 / 0.726026fluid inclusions in mineralised quartz (present-day ratio)
Mean and standard deviation recalculated from 6 analyses, 0.71774 to 0.72602 (ck250 0.72602; ck262 0.71897; ck266 0.71847; ck288 0.71774; ckl165 0.72162; ckl197 0.71808). Table 4 (1σ uncertainty on the last digits): ck250 (Rb 0.2819, Sr 0.0801 ppm, 87Rb/86Sr 10.166, 87Sr/86Sr 0.72602 ± 2); ck262 (Rb 0.6859, Sr 0.8421 ppm, 87Rb/86Sr 2.3150, 87Sr/86Sr 0.71897 ± 2); ck266 (Rb 2.5124, Sr 3.3738 ppm, 87Rb/86Sr 1.9409, 87Sr/86Sr 0.71847 ± 2); ck288 (Rb 0.5136, Sr 1.4183 ppm, 87Rb/86Sr 1.0451, 87Sr/86Sr 0.71774 ± 2); ckl165 (Rb 1.528, Sr 0.906 ppm, 87Rb/86Sr 4.871, 87Sr/86Sr 0.72162 ± 9); ckl197 (Rb 0.945, Sr 1.754 ppm, 87Rb/86Sr 1.554, 87Sr/86Sr 0.71808 ± 7). Isochron of 68 ± 6 Ma (MSWD 4.14); present-day ratios, not age-corrected. Sr standard not given in the paper.
Liang et al. (2007), Geology and geochemistry of the adjacent Changkeng gold and Fuwang s…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Fuwang, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/fuwang/ (accessed 2026-10-21).

@misc{isofind2026fuwangisotopesignatures,
  title = {Fuwang, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/fuwang/},
  note = {Accessed 2026-10-21}
}

Updated : 2026-10-21