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Tongshankou

Hubei, Middle-Lower Yangtze belt, China

PorphyriesCu-Au-Mo

Type
Porphyry Cu-Au (Mo)

High-Mg adakitic pluton (granodiorite porphyry and granodiorite, 140 to 137 Ma) hosting porphyry Cu-Au (Mo) mineralization, in Silurian to Triassic clastic rocks. Fan et al. (2020): whole-rock δ11B from -12.53 to -9.82 ‰.

δ11B in ‰ (per mil) Values of the same system

Standard : NIST SRM 951

ValueRangenMineral or matrixSource
−12.53 / −9.82 ‰whole rock, granodiorite porphyry and granodiorite
Range only. 4.62 to 5.74 ppm B. The 16 rocks of the Middle-Lower Yangtze have δ98/95Mo from -0.5 to +0.2 ‰, not split by deposit.
Fan et al. (2020), Molybdenum and Boron Isotopic Compositions of Porphyry Cu Mineralizati…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Tongshankou, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/tongshankou/ (accessed 2026-10-20).

@misc{isofind2026tongshankouisotopesignatures,
  title = {Tongshankou, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/tongshankou/},
  note = {Accessed 2026-10-20}
}

Updated : 2026-10-20