Last Updated:2025/12/08

closure temperatures help geologists determine when minerals last cooled below the point where isotopes become locked in.

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closure temperatures help geologists determine when minerals last cooled below the point where isotopes become locked in.

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閉鎖温度は、鉱物が同位体を閉じ込める温度を下回って最後に冷却した時期を地質学者が特定するのに役立ちます。

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