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Barneys Canyon and Melco (Bingham district)

Utah, Oquirrh Mountains, United States

Other hydrothermalAu

Type
Sediment-hosted disseminated gold (Carlin type)

Disseminated gold deposits about 7 km north of the Bingham Canyon porphyry, in brecciated, clay-altered quartzites and limestones; the most scattered ε205Tl ever observed in a hydrothermal system (-16.4 to +6.0), anomalies linked to Tl-Sb-As-enriched breccias and low-temperature fluids according to Fitzpayne et al. (2018). Indicative coordinates, derived from the distance to Bingham Canyon.

ε205Tl in ε units (parts per 10,000) Values of the same system

Standard : NIST SRM 997

ValueRangenMineral or matrixSource
−4 ± 8.32 ε−16.4 / 6 ε5stockwork limestone, brecciated quartzites, quartzite and dolomitic nodule (whole rock)
Mean and standard deviation recalculated from 5 analyses, BC11MB185 (quartzite breccia, -16.4) and BC11MB184 (collapse breccia near the Melco pit, +6.0) at the extremes; veined limestone BC11CW089b at 31,590 ng/g Tl.
Fitzpayne et al. (2018), Assessing Thallium Elemental Systematics and Isotope Ratio Varia…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Barneys Canyon and Melco (Bingham district), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/barneys-canyon-et-melco-district-de-bingham/ (accessed 2026-10-15).

@misc{isofind2026barneyscanyonandmelcobinghamd,
  title = {Barneys Canyon and Melco (Bingham district), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/barneys-canyon-et-melco-district-de-bingham/},
  note = {Accessed 2026-10-15}
}

Updated : 2026-10-15