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Non-destructive energy dispersive x-ray fluorescence analysis was applied to obsidian flakes from 25LP8, a Lower Loupphase site in Nebraska. All flakes have the same trace element composition as volcanic glasses of the Cerro del Media chemical type, located in the Jemez Mountains of northern New Mexico.
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Stored only when both papers are in the corpus — 8 citations exist upstream.
Papers that cite the same references — the relational fallback while embeddings are still backfilling.
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