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来自圣多美 (喀麦隆火山线) 火山气体排放中的贵重气体同位素的HIMU地幔源的表征
Arno Lastes1, David V Bekaert1, Bouchaib Tibari1
1Université de Lorraine, CNRS, CRPG, 54000 Nancy, France.
概括
圣多美火山活动的源头是一个类似羽毛状的地幔水库,与中洋基岩相比,它富含虹同位素. 这项研究使用了贵重气体同位素来研究地幔组成部分和潜在的回收地影响.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 火山学 火山学是一门学科.
背景情况:
- 喀麦隆火山线沿着火山活动的起源尚未完全理解.
- 地幔羽毛-石相互作用和地循环是地幔异质性的关键因素.
研究的目的:
- 为了研究圣多美岛火山活动的地幔源组成部分.
- 在地幔衍生气体中分析轻 (He-Ne-Ar) 和重 (Kr-Xe) 贵气同位素.
- 为了限制回收地物质在地幔中的作用.
主要方法:
- 高精度动态质谱 (DMS) 用于贵重气体同位素分析.
- 测量了,,,,,和的同位素比例.
- 对同位素进行了对地表扩散运输分离的校正.
主要成果:
- 圣托马斯的火山起源于一个类似羽毛状的地幔储层,与对流的上层地幔 (MORB) 不同.
- 离子同位素 (Ne/Ne) 显示在圣多美羽毛源中的缩.
- 轻微过多的136Xe,归因于238U裂变,表明地幔源中的回收地成分.
结论:
- 圣多美地幔的来源是羽毛状的,有循环地物质的证据可能与HIMU型地幔有关.
- 在不同的地幔储库中观察到的129Xe/136Xe的同质性挑战了现有的同位素演化模型.
- 需要进一步的研究,以了解与其他挥发性元素相比,均的129Xe/136Xe比的含义.
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