まとめ
地球 地球 地球 地球 地球
科学分野:
- 地質化学 地質化学
- 宇宙化学 (コスモケミストリー)
- ラジオメトリック・デッティング
背景:
- 過去の地球年齢の計算では,鉄隕石と現代の地上の鉛からの鉛同位体比を用いた.
- 最近のデータでは,現代の陸上の鉛の同位体多様性が広く示され,以前の仮定に異議を唱えている.
研究 の 目的:
- 地球の年齢を再計算するには,以前の放射線年代測定法で違反した仮定に対処する必要があります.
- 鉛の同位体変動が地球の年齢決定に及ぼす影響を調査する.
主な方法:
- 鉄隕石の鉛と27億年前のカナダ盾の岩を比較して,鉛同位体解析を修正しました.
- 以前の年齢計算から得られた既定の定数と仮定を利用した.
主要な成果:
- 改訂された地球の年齢を4750 ±5千万年と計算した.
- これは,地球が以前に推定されたよりも約2億年年上である可能性を示唆しています.
結論:
- 地球の年齢は45億5500万年より古いかもしれません.
- 不一致は,鉄隕石と比較して,原始的な地上の鉛の同位体組成の変動から生じる可能性があります.
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