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Taylor Creek

Black Range, New Mexico, United States

Epithermal depositsSn

Type
Wood tin in rhyolite domes

Oligocene (about 28 Ma) rhyolite-hosted tin district: veinlet cassiterite in rhyolite domes, deposited by vapour-rich, halogen-bearing fluids in a shallow setting. Indicative coordinates.

δ124Sn in ‰ (per mil) Values of the same system

Standard : NIST SRM 3161a

ValueRangenMineral or matrixSource
−0.38 ± 0.74 ‰−1.23 / 0.1 ‰3cassiterite
Mean and standard deviation recalculated from 3 samples, Table 2. Ore age used by the authors: 28 Ma.
Mathur et al. (2025), Global Sn isotope compositions of cassiterite identify the magmatic…
−0.48 ± 0.65 ‰−1.18 / 0.81 ‰11cassiterite (wood tin), single grains
Mean and standard deviation recalculated from 11 samples, Table 4. Minus signs missing from the extracted text, restored from the page image. Partly reproduced by Mathur et al. (2025).
Wang et al. (2019), Experimental evidence for fractionation of tin chlorides by redox and…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Taylor Creek, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/taylor-creek/ (accessed 2026-10-13).

@misc{isofind2026taylorcreekisotopesignatures,
  title = {Taylor Creek, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/taylor-creek/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13