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Pike Hill mine (Vermont)

Vermont, Orange County (Corinth), United States

Volcanogenic massive sulfidesCu-Zn

Type
Besshi-type massive sulfides (Cu-Zn) in metasediments

Cu-Zn deposit of Devonian (?) age in a dominantly clastic metasedimentary terrane, metamorphosed to amphibolite facies. Palmer and Slack (1989, Table 1): tourmaline at -13.88 ‰. Tourmalines of this kind of terrane range from -15.37 to -2.19 ‰ in the article; according to the authors, the boron source (continental crust, entrained seawater, evaporites) matters more than the formation temperature.

δ11B in ‰ (per mil) Values of the same system

Standard : NIST SRM 951

ValueRangenMineral or matrixSource
−13.88 ‰1tourmaline of the massive sulfide or associated tourmalinite
Single analysis (PH-810-9). Uncertainties: PH-810-9 -13.88 ± 0.35 ‰ (repeat -13.80 ± 0.34 ‰, not averaged).
Palmer & Slack (1989), Boron isotopic composition of tourmaline from massive sulfide depo…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Pike Hill mine (Vermont), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/mine-de-pike-hill-vermont/ (accessed 2026-10-19).

@misc{isofind2026pikehillminevermontisotopesig,
  title = {Pike Hill mine (Vermont), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/mine-de-pike-hill-vermont/},
  note = {Accessed 2026-10-19}
}

Updated : 2026-10-19