石中的238U/235U变化:现存的247Cm和对Pb-Pb约会的含义
G A Brennecka1, S Weyer, M Wadhwa
1School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287, USA. brennecka@asu.edu
概括
石中的同位素比率不是恒定的,这挑战了太阳系年龄计算的准确性. 富含和的含量变化表明约会方法可能会高估数百万年的年龄.
科学领域:
- 宇宙化学 宇宙化学
- 地质时间学 (Geochronology)
- 核天体物理学 核天体物理学
背景情况:
- -238/-235 (238U/235U) 同位素比率在石中被认为是恒定的.
- 这种假设是确定太阳系年龄的高精度-年龄测定的基础.
研究的目的:
- 研究石材料中238U/235U同位素比率的变化.
- 重新评估这些变化对太阳系时间表的影响.
主要方法:
- 分析来自阿伦德石的富含含量含量 (CAI).
- 对238U/235U同位素比的测量.
- 同位素变化的相关性与/ (Th/U,Nd/U) 的代理值.
主要成果:
- 在CAI中观察到的变量238U/235U比率,范围从137.409到137.885.
- 鉴定了CAI年龄的潜在高估数百万年,这是由于约会的不确定性.
- 强有力的证据将238U/235U变异与-247 (247Cm) 到-235 (235U) 的衰变联系起来.
结论:
- 在早期太阳系的初始247Cm/235U比率大约是1.1×10−4到2.4×10−4.
- 247Cm的衰变是影响早期太阳系材料中238U/235U比率的重要因素.
- 需要重新评估CAI的-测年.
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