来自拉马克花岩的证据表明,加利福尼亚州的晚白纪快速地形成
概括
和的同位素揭示了塞拉内华达山脉中拉马克侵入性套件的宝石起源于一个丰富的地幔来源. 这一发现表明,在美国的白时期的岩石形成过程中,有显著的青少年地增加.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 石化学 石化学是一门学科.
背景情况:
- 塞拉内华达巴索利石是北美山脉的主要组成部分.
- 了解其石化形成是解读地生长过程的关键.
- 拉马克侵入性套件代表了巴托利特内部的一个重要的岩事件.
研究的目的:
- 为了调查拉马克侵入性套房的起源和演变.
- 评估地幔来源在塞拉内华达巴索利石形成中的作用.
- 改进美国西部地生长率的估计.
主要方法:
- 在加布洛岩石和花岩石中分析和的同位素.
- 拉马克入侵套房的地化学特征.
- 同位素数据与已知的地幔和地水库的比较.
主要成果:
- 同位素数据 (和) 在拉马克套件的组成光谱中显示最小的变化.
- 布罗的侵入产生了相同的同位素特征,这与来自丰富的地幔源的衍生一致.
- 这些发现挑战了关于该地区地生长的先前假设.
结论:
- 拉马克侵入套件很可能是从丰富的地幔源形成的,这表明地幔局部参与.
- 这种参与需要对美国地生长率估计进行修订.
- 塞拉内华达巴索石的部分可能代表了白纪期间形成的主要是青少年地.
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