在古磁记录中检测地磁场的二极性
Florian Lhuillier1, Valeriy P Shcherbakov2, Natalia K Sycheva2
1Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universitaet, 80333 Munich, Germany.
概括
了解过去的地磁场强度对于地球科学至关重要. 我们的分析显示了场强度和倾斜之间的相关性,提高了地球古磁记录的可靠性.
科学领域:
- 地质物理学 地质物理学
- 地球科学 地球科学 地球科学
- 古磁力学是一种古磁学.
背景情况:
- 地磁场强度恢复对于理解地球的深层动力学和地磁场系统至关重要.
- 古磁记录为地球过去的磁场行为提供了见解.
研究的目的:
- 分析地磁场强度和倾向之间的关系,以增强古磁记录的预测能力.
- 为了研究不同地质时间尺度之间的相关性的重要性.
主要方法:
- 对地磁场模型的统计分析.
- 考察古磁数据,包括古强度和古方向.
- 严格过器对古磁数据的应用,以进行质量控制.
主要成果:
- 对于类似地球的磁场,即使有噪音和变化,也观察到地磁场强度和倾斜度之间的显著相关性.
- 由于采样问题,对于布鲁尼斯极性时间来说,这种相关性并不显著.
- 从1到130万年前发现了显著的相关性,在严格的数据过的情况下,在130万年前发现了微小的相关性.
结论:
- 甲纪正常超时似乎与增强的地球气相双极性无关.
- 在130万年前的古代地磁场,可能与今天的地磁场平均不大不同.
- 由于有限的高质量的古磁数据,检测前坎布里亚时期的地磁模系统具有挑战性.
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