在地幔过渡区的原始和循环同位素特征
S Timmerman1, M Honda2, A D Burnham2
1Research School of Earth Sciences, Australian National University, 142 Mills Road, Acton, ACT 2601, Australia. suzette.timmerman@anu.edu.au.
概括
在超深层钻石中测量了深层地幔同位素特征. 低排气,高-3/-4深层地幔源透到过渡区,影响着玄武岩的组成.
科学领域:
- 地质化学
- 地质学
- 石油学
背景情况:
- 岩同位素的组成揭示了地球内部的化学储备.
- 直接测量深层地幔同位素是一个挑战.
- 了解深层地幔对于解释喷发的玄武岩痕迹至关重要.
研究的目的:
- 在超深的钻石液体内测量 (He), (Sr) 和 (Pb) 的同位素比率.
- 为了研究深层地幔的同位素信号.
- 了解海洋岛屿玄武岩的同位素变化的起源.
主要方法:
- 来自过渡区 (410660公里深度) 的钻石中的液体含量对He-Sr-Pb同位素的分析.
- 使用超深钻石作为原始样本,不受脱气和地污染的影响.
主要成果:
- 观察到极端的He-C-Pb-Sr同位素变异性.
- 确定高的3He/4He比率与度的升高相关.
- 表明存在较少的脱气,高3He/4He深层地幔来源.
结论:
- 一个高3He/4He的深层地幔源透到过渡区.
- 这种深层来源与过渡区的回收材料之间的相互作用会产生同位素多样性.
- 这一过程解释了海洋岛基岩中发现的多样化的同位素组成.
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