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Furnace Bed (Pikes Peak mine)

New Jersey Highlands, United States

OtherFe

Type
Silicate-poor magnetite hosted 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
−2.21 ± 3.08 ‰−4.39 / −0.04 ‰2calcite of the ore-hosting marble
Mean and standard deviation recalculated from 2 samples, Table 3. Magnetite layer beneath the Franklin zinc orebody; FB-1 and FR-1 (Pikes Peak).
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
14.33 ± 2.76 ‰12.38 / 16.28 ‰2calcite of the ore-hosting marble
Mean and standard deviation recalculated from 2 samples, Table 3. Magnetite layer beneath the Franklin zinc orebody; FB-1 and FR-1 (Pikes Peak).
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). Furnace Bed (Pikes Peak mine), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/furnace-bed-mine-pikes-peak/ (accessed 2026-10-13).

@misc{isofind2026furnacebedpikespeakmineisotop,
  title = {Furnace Bed (Pikes Peak mine), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/furnace-bed-mine-pikes-peak/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13