洪水-玄武岩起源的古老配方
Matthew G Jackson1, Richard W Carlson
1Department of Earth Sciences, Boston University, 675 Commonwealth Avenue, Boston, Massachusetts 02215, USA. jacksonm@bu.edu
Nature
|July 29, 2011
概括
大规模的洪水玄武岩,如通爪高原,起源于一个古老的,原始的地幔水库. 这种地球深处的源泉存在了45亿年,影响了地球上最大的火山事件的发生.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 地球科学 地球科学 地球科学
背景情况:
- 大量的玄武岩喷发 (洪水玄武岩) 是重要的地质事件.
- 产生如此巨大的融化体积的来源和机制仍然不太清楚.
- 一个早期形成的地幔水库,可能有45亿年历史,已被提出为一些洪水玄武岩的来源.
研究的目的:
- 为了调查大批洪水玄武岩的起源.
- 确定拟议的古代地幔水库是否是主要火山事件的广泛来源.
- 了解这个原始地幔源在洪水玄武岩生成中的作用.
主要方法:
- 对玄武岩样本进行地质化学分析.
- 同位素和微量元素特征分析.
- 来自各种大型火山省份的地化学数据的比较.
主要成果:
- 来自通爪高原的岩石表现出与拟议的早期地球地幔水库相一致的地化学特征.
- 在过去的2.5亿年里,有六个主要的火山事件共享了这些签名,表明一个共同的古老源头.
- 这座古老的水库的特点是由于大量的产生热量的元素,温度更高,肥沃度更高.
结论:
- 最古老的陆地地幔水库是多次大规模洪水玄武岩事件的重要来源.
- 这个原始地幔水库的地化学特性 (更热,更肥沃) 是产生大规模火山爆发的关键因素.
- 这一发现为地幔演变的动态和地球历史上大规模的岩石流提供了至关重要的见解.
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