16 From Thin Section to Outcrop: Exploration of Undergraduate Research (Posters)
This session is designed to showcase undergraduate research across all disciplines. All submissions should be written by the student(s) and include a faculty co-author. Categories: Cross-Disciplinary, all topics welcome
Sunday, 22 March 2026
1:30 PM - 5:30 PM
CCC, Ballroom C
Analysis of Titanite from the Oak Hill Wollastonite Deposit, Eastern Adirondacks
Paper number: 16-40
Program: Technical Sessions
Time: 1:30 PM – 1:30 PM
Authors
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Christian SchraderSUNY-Potsdam, Potsdam, NY
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Taylor KellnSuwanee, GA
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EveNYCO, Lewis, NY
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Parker LeClairLewis, NY
Abstract
Wollastonite skarn deposits in the eastern Adirondacks record multiple thermal events during the Grenville orogeny. Wollastonite is a valuable industrial mineral with a notable acicular crystal habit that is used as a versatile, functional filler and reinforcing agent in plastics, paints, and ceramics. In this study, we attempt to characterize the thermal history of the Oak Hill wollastonite deposit (Lewis, NY) using titanite. Samples were collected from the pit and analyzed at the Arizona LaserChron Center for U-Pb dating and LA-ICPMS titanite mineral chemistry. Thirty-five spots were analyzed. Additional samples from drill core were examined petrographically.
Previous work on these deposits using zircon (e.g., Peck et al. 2025, J. Petrol. 66:4) showed distinct age populations corresponding to known thermal events in Adirondack geological history, i.e., Shawinigan, AMCG, Ottowan, and Rigolet. Our titanite ages show either heterogeneous Pb incorporation or, perhaps more likely, Pb-loss. A Tera-Wasserburg plots yields a weighted mean age of 948.9 +/-3.7 Ma, which is best viewed as a minimum rather than a true formation age. The titanites appear homogeneous across samples: titanite grains show no zonation in electron backscatter imaging or within the laser ablation data. On a chondrite-normalized REE plot they all show distinct negative Nd-anomalies and negative Eu-anomalies, the latter presumably due to the ircrystallization in the presence of abundant plagioclase.
Geological Society of America Abstracts with Programs. Vol. 58, No. 2
doi: 10.1130/abs/2026NE-411381
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