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Sulphur Hill mine

New Jersey Highlands, United States

OtherFe

Type
Skarn-hosted magnetite in marbles

Small magnetite deposit in Mesoproterozoic marbles of the New Jersey Highlands, metamorphosed in Grenvillian times. The authors see Fe oxides and hydroxides brought by a back-arc submarine hydrothermal system (1.3 to 1.25 Ga), the same as for the zinc at Franklin and Sterling Hill. Coordinates from the publication.

δ13C in ‰ (per mil) Values of the same system

Standard : V-PDB

ValueRangenMineral or matrixSource
−3.73 ± 0.4 ‰−4.2 / −3.5 ‰3calcite of the magnetite skarn
Mean and standard deviation recalculated from 3 samples, Table 3. Data from Meredith et al. (2003), reproduced in the table.
Peck et al. (2009), Stable isotope and petrologic evidence for the origin of regional mar…

δ18O in ‰ (per mil) Values of the same system

Standard : V-SMOW

ValueRangenMineral or matrixSource
13.27 ± 0.81 ‰12.7 / 14.2 ‰3calcite of the magnetite skarn
Mean and standard deviation recalculated from 3 samples, Table 3. Data from Meredith et al. (2003), reproduced in the table.
Peck et al. (2009), Stable isotope and petrologic evidence for the origin of regional mar…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Sulphur Hill mine, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/mine-sulphur-hill/ (accessed 2026-10-13).

@misc{isofind2026sulphurhillmineisotopesignatu,
  title = {Sulphur Hill mine, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/mine-sulphur-hill/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13