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Updated: Jul 11, 2026

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Negative Additive Manufacturing of Complex Shaped Boron Carbides
Published on: September 18, 2018
概括
海洋岛屿基岩具有一致的同位素比率. 相比之下,中洋山脊玄武岩和后弧盆地玄武岩显示出更高,变化的比率,可能是由于地同化.
科学领域:
- 地质化学 地质化学
- 同位素地球化学 同位素地球化学
- 石化学 石化学是一门学科.
背景情况:
- 火山玻璃中的同位素比例为地球地幔和地过程提供了洞察力.
- 大洋岛基岩 (OIBs) 呈现出均的同位素组成,而中洋山脊基岩 (MORBs) 和后弧盆地基岩 (BABBs) 则显示出更大的变异性.
研究的目的:
- 调查不同基岩类型中观察到的不同同位素比率背后的原因.
- 为了确定地同化对地幔衍生的融物中的同位素特征的影响.
主要方法:
- 从OIB,MORB和BABB的火山玻璃中分析同位素比率.
- 在地幔分化和地同化过程中的同位素分化的建模.
主要成果:
- 来自OIB的火山玻璃始终显示波同位素比率约为每毫米 -9.9 ± 1.3 (相对于NBS 951).
- 在MORB和BABB中,同位素的比率更高,变化更大.
- 即使是变化的玄武岩地的微小同化也会显著改变融中的同位素比率.
结论:
- 地同化是导致MORBs和BABBs中同位素比率升高和变化的主要因素.
- 原始地幔可能具有每毫米 -10 ± 2 的同位素比率.
- 在重要的地幔分化过程中,同位素的比率一直保持相对不分化.
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