34 Conventional and Unconventional Critical Mineral Resources in the Eastern United States (Posters)
Saturday, 18 March 2023
1:30 PM - 5:30 PM
Grand Ballroom A–D
CRITICAL MINERAL POTENTIAL OF PEGMATITES: HOW CLASSIFYING THEIR ZONATION CAN INFORM EXPLORATION
Paper number: 34-4
Program: Theme Sessions
Time: 1:30 PM – 5:30 PM
Authors
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Finn O'NeilFurman University, Greenville, SC
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Emma HuntFurman University, Greenville, SC
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Ruth AronoffFurman University, Greenville, SC
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William RansonFurman University, Greenville, SC
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Nigel KellyMadison, SC
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Peter HorvathFurman University, Greenville, SC
Abstract
The Helen Beryl pegmatite has enrichment in beryl and spodumene, which can be well categorized by a geochemical classification such as LCT (lithium-cesium-tantalum). In contrast, the Ray pegmatite, Spruce Pine region, North Carolina, has unusual mineral wealth including columbite-group, lepidolite, beryl, fluorite, elbaitic tourmaline, amazonite, pollucite, and apatite that cannot be adequately classified into a single geochemical group. Micro-XRF analysis of one sample from the Ray pegmatite revealed the complexity of the zonation at Ray with a single columbite-group crystal displaying a Nb-rich core and Ta-rich rim. These data indicate that, at least at Ray, pegmatites are better classified by the accessory mineral scheme of Wise et al. (2022). The Ray pegmatite is a product of residual melt of granitic magmatism (RMG), group 1 type. The value of researching the mineralogy present and accurately classifying pegmatites is key for understanding the resources within these that may help supply the critical minerals for the energy transition.
Geological Society of America Abstracts with Programs. Vol. 55, No. 2
doi: 10.1130/abs/2023SE-385524
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