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黑马-伊尔梅尼特系列中的板状磁性作为强残余磁化强的解释
Peter Robinson1, Richard J Harrison, Suzanne A McEnroe
1Geological Survey of Norway, N-7491, Trondheim, Norway. peter.robinson@ngu.no
Nature
|August 2, 2002
概括
铁-氧化物中的一个新的磁基结构解释了火山岩中异常强大的残留物. 这一发现涉及铁接触层,揭示了地质材料增强磁性质的机制.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 岩石磁力 岩石磁力 岩石磁力
背景情况:
- 火性岩石和变态岩石中的磁性异常通常与磁石有关.
- 中间的伊尔梅尼特-黑马提特系列矿物质可以携带强烈的残留物,但它通常只在快速冷却的火山岩中保存.
- 在岩石中观察到异常大且稳定的残留物,这些岩石具有伊尔梅尼特 - 黑马提特的交长,但没有完全解释.
研究的目的:
- 调查含有伊尔梅尼特-黑马杂生长的火山岩中异常强大和稳定的自然残留磁化的原因.
- 提出一个新的磁基结构,以解释观测到的高磁残.
主要方法:
- 在铁-氧化阶段对溶解膜的分析.
- 纳米级 (低至1nm) 磁基结构的理论建模.
- 基于拟议的模型估计和磁化.
主要成果:
- 观测到的溶解片的厚度从100微米到1纳米不等.
- 提出了一个新的铁磁基结构,涉及黑铁"接触层"之间的血和伊尔梅尼特.
- 估计和磁化高达55kA m(-1),明显高于纯血,同时保持高强制性.
结论:
- 拟议的铁-铁"接触层"为在某些火山岩中观察到的异常强的残余磁化提供了一个机制.
- 这种子结构解释了氧化物含量较小的岩石如何表现出显著的磁异常.
- 这些发现对理解地质记录中的磁性签名和潜在的磁性材料应用有意义.
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