Fule

Yunnan (Pb-Zn-Cd district), China

Mississippi Valley TypeZn-Pb-Cd

Type
Mississippi Valley Type (MVT)

MVT deposit rich in cadmium, with supergene alteration. Dark and light sphalerites have contrasting cadmium compositions, and the δ114/110Cd of supergene smithsonite increases with maturity.

δ114/110Cd in ‰ (per mil) Values of the same system

Standard : NIST SRM 3108

ValueRangenMineral or matrixSource
0.06 / 0.46 ‰dark sphaleriteWen et al. 2016, Cd isotope fractionation in Fule MVT (Mineralium Deposita)
0.43 / 0.7 ‰light sphaleriteWen et al. 2016, Cd isotope fractionation in Fule MVT (Mineralium Deposita)
−0.35 / 0.39 ‰galena (sphalerite micro-inclusions)Wen et al. 2016, Cd isotope fractionation in Fule MVT (Mineralium Deposita)
0.19 / 0.42 ‰supergene smithsoniteWen et al. 2016, Cd isotope fractionation in Fule MVT (Mineralium Deposita)

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Fule, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/fule/ (accessed 2026-10-06).

@misc{isofind2026fuleisotopesignatures,
  title = {Fule, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/fule/},
  note = {Accessed 2026-10-06}
}

Updated : 2026-10-06