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Magnetic Tweezers for the Measurement of Twist and Torque
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在过去的200万年里,地磁双极强度和逆转率
Jean-Pierre Valet1, Laure Meynadier, Yohan Guyodo
1Géomagnétisme et Paléomagnétisme (UMR CNRS 7577), Institut de Physique du Globe de Paris, 4 Place Jussieu, 75252 Paris Cedex 05, France. valet@ipgp.jussieu.fr
Nature
|June 10, 2005
概括
在200万年间地磁双极时刻的演变显示,在非反转时期,磁场更强. 这项研究为地磁场过程和地磁场行为提供了新的见解.
科学领域:
- 地质物理学 地质物理学
- 古磁论是古磁论的一种学说.
- 地球科学 地球科学 地球科学
背景情况:
- 地磁二极子时刻的演变对于理解地磁多摩过程至关重要.
- 以前的重建仅限于过去的80万年,不包括地磁逆转.
研究的目的:
- 为了重建地磁双极时刻在过去200万年的演变.
- 为了研究双极时刻强度和地磁反转之间的关系.
主要方法:
- 从全球沉积物核心堆叠相对古老强度的独立记录.
- 校准复合曲线与来自火山岩的绝对二极极时刻.
主要成果:
- 在过去200万年的地磁双极时刻的复合曲线被生成.
- 在没有逆转的时期,时间平均场较强.
- 轴性双极在逆转之前衰减60-80 kyr,然后在相反的方向上迅速重建.
结论:
- 较强的平均二极子时刻与较少的地磁不稳定性相关,如游览和反转.
- 地磁场的行为,包括反转,与平均磁场强度有关.
- 这项研究扩展了我们对地力学动力学过程的理解,使我们更进一步地追溯到过去.
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