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Orphan Lode (Grand Canyon)

Arizona, Coconino County, South Rim of the Grand Canyon, United States

UraniumU (Cu)

Type
Uranium-bearing collapse breccia pipe

Circular vertical collapse breccia pipe in Pennsylvanian and Permian limestones of the Arizona Strip, uranium concentrated in the matrix and fractures, Late Triassic mineralisation; fluid inclusions at 80 to 170 °C and 9 to 19 wt% NaCl eq. from secondary sources cited by Balboni et al. (2016); highest 87Sr/86Sr ratio of the study. Uraninite 87Sr/86Sr measured by Balboni et al. (2016) for nuclear forensics: low ratios (below 0.7200) in low-temperature sandstone deposits, high in pegmatites, veins and breccia pipes. Coordinates from Mindat.

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

Standard : NIST SRM 987

ValueRangenMineral or matrixSource
0.76288 ± 0.0000121breccia pipe uraninite
Single analysis; value read from the Figure 7 label, 2σ uncertainty; highest ratio of the study.
Balboni et al. (2016), Chemical and Sr isotopic characterization of North America uranium…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Orphan Lode (Grand Canyon), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/orphan-lode-grand-canyon/ (accessed 2026-10-15).

@misc{isofind2026orphanlodegrandcanyonisotopes,
  title = {Orphan Lode (Grand Canyon), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/orphan-lode-grand-canyon/},
  note = {Accessed 2026-10-15}
}

Updated : 2026-10-15