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月球上长期存在的KREEP岩,由最年轻的月球岩火岩岩所表明
Lars E Borg1, Charles K Shearer, Yemane Asmerom
1Institute of Meteoritics, Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA. lborg@unm.edu
Nature
|November 13, 2004
概括
新的分析显示,月球上的,稀土元素和 (KREEP) 岩持续了10亿年. 这一发现基于最年轻的月球样本,扩大了我们对月球地质历史的理解.
科学领域:
- 月球地质学 月球地质学
- 星球科学 星球科学
- 石化学 石化学是一门学科.
背景情况:
- 月球的组成多样性源于其岩海洋的原始固化和融化.
- 早期的月球岩石含有丰富的橄烯和火烯,其次是富含原酸的岩石.
- ,稀土元素和 (KREEP) 材料是在海的最后结晶阶段形成的.
研究的目的:
- 为了调查月球上的KREEP岩的持续时间和程度.
- 为了确定KREEP是否参与了最近的月球岩活动.
- 为了分析最年轻的月球样本,寻找KREEP的证据.
主要方法:
- 对最年轻的月球样本进行分析.
- 月球样本的地化学和时间分析.
- 射线测年技术. 射线测年技术.
主要成果:
- 有证据表明,KREEP的岩石流延长了10亿年,超出了先前确定的时间表.
- 最年轻的月球样本显示了KREEP岩的特征.
- 这延长了月球上已知的KREEP相关地质活动时期.
结论:
- 克里普岩活动的持续时间比以前认为的要长.
- 这些发现挑战了现有的月球热进化和岩石运动模型.
- 这种延长的岩活动对了解月球的内部热源和地质演变有意义.
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