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Experimental data investigates the alkali-silica reactivity (ASR) of aggregates from İstanbul’s Thrace Formation. The dataset includes results from mineralogical, thermal, and ASTM C1260 expansion analyses to demonstrate how a short 800°C/7-minute treatment mitigates ASR by partially dehydroxylating clay minerals. Findings show reduced expansion and altered ASR gel chemistry, supporting aggregate-level modification as a practical mitigation pathway.
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