在上层地幔中广泛存在的PREMA,由低度的玄武岩融表明
Ronghua Cai1, Jingao Liu2, D Graham Pearson3
1State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing, 100083, China.
Nature communications
|December 9, 2023
概括
在玄武岩中发现的普遍地幔 (PREMA) 成分是高度可融的,可能起源于地球历史的早期. 这表明PREMA在上层地幔中普遍存在,而不仅仅与深层地幔羽毛有关.
科学领域:
- 地质化学 地质化学
- 世界地幔地力学地力学
- 石化学 石化学是一门学科.
背景情况:
- 主流地幔 (PREMA) 组件是地幔地化学阵列的关键特征.
- 它的起源和分布仍然存在争议,有建议与深层地幔羽毛和低剪波速度省 (LLSVPs) 的联系.
研究的目的:
- 调查PREMA组件的来源和分布.
- 分析中纪海洋和大陆基岩的组成系统学.
主要方法:
- 分析了大约3500个中生代海洋和大陆基岩.
- 地化学建模. 地化学建模.
- 地幔对流模拟.地幔对流模拟.
主要成果:
- 低度基岩融具有高度的Nb度,在深层地幔羽毛之外发现,表现出类似PREMA的Sr-Nd-Hf同位素特征.
- 普雷玛具有高度的融合性,并且不仅仅与LLSVP有关.
- 地化学和对流模型表明,PREMA是在地球历史的早期形成的,变化最小.
结论:
- PREMA很可能起源于地球积聚后不久.
- 它分散在整个上层地幔中,而不是由枯竭和丰富的地幔成分混合而产生的.
- 这挑战了PREMA与深层地幔羽毛的独家关联.
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