Isotope and trace element data from skarns from the Lewis wollastonite deposit, Adirondack Highlands, New York
Abstract:
This dataset of minerals from low-δ18O skarn rocks in the Lewis wollastonite deposit has the aim of constraining the timing of surface-derived meteoric water infiltration during skarn formation. U-Pb and trace element data were measured by laser-ablation ICP-MS. Oxygen isotopes were measured by ion microprobe (zircon) and laser fluorination (other minerals).
How to cite this dataset:
Peck, W. H., Regan, S. P., Blum, T. B., Valley, J. W., Timothy, S. C., 2026. Isotope and trace element data from skarns from the Lewis wollastonite deposit, Adirondack Highlands, New York, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA).
https://doi.org/10.60520/IEDA/113500. Accessed 2024-12-26.
DOI Creation Date:
2024-10-21
Related
Publication(s):
Peck, William H., Regan, Sean P., Blum, Tyler B., Valley, John W., and Timothy, Samuel C., Age of skarn formation and meteoric water infiltration in the Willsboro-Lewis wollastonite district (Adirondack Highlands, New York), Journal of Petrology, submitted.
License:
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Funding source(s):
Colgate University
National Science Foundation:
2136782 European Union’s Horizon 2020 research and innovation program grant agreement 856555
Keyword(s):
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Adirondack Mountains, Essex County, New York
User Contributed Keyword(s):
massif anorthosite; wollastonite skarn; zircon; geochronology; oxygen isotopes
Data Available On:
2026-10-10