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Updated: May 1, 2026

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Magnetic Tweezers for the Measurement of Twist and Torque
Published on: May 19, 2014
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摩托诺里·马图亚马 (Motonori Matuyama) 和地磁场的逆转
1Professor Emeritus, Tokyo Institute of Technology, Tokyo, Japan.
概括
由火山岩磁化定义的马图亚马时代标志着早期的四度纪时期. 它的下限现在被用来定义四年纪地质时代的开始.
科学领域:
- 古磁论是古磁论的一种学说.
- 地质时间学 (Geochronology)
- 地球科学 地球科学 地球科学
背景情况:
- 对地球磁场逆转的研究对于理解地质历史至关重要.
- 20世纪初,马图亚马对火山岩磁化的研究奠定了基础概念.
- 20世纪中叶的研究确立了地磁极性时间表.
研究的目的:
- 要总结古磁研究的历史发展.
- 定义关键的地磁极性时代,包括马图亚马时代.
- 为了突出马图亚马时代的下极限在定义四季纪时期的意义.
主要方法:
- 火山岩石的古磁测量. 火山岩石的古磁测量.
- 火山形成的放射测年法. 火山形成的放射测年法.
- 磁极性的相关性与地质时间的反转.
主要成果:
- 马图亚马时代的跨度从0.773万年前到2.595万年前.
- 马图亚马时代的下界被认为是四年纪的开始.
- 已确立的地磁极性时代 (布伦赫斯,马图亚马,高斯,吉尔伯特) 仍然被广泛使用.
结论:
- 对火山岩的古磁性研究对重建地球历史起了重要作用.
- 马图亚马时代作为地质时间表中的一个关键标记.
- 极性时代的历史命名惯例在当代科学文献中仍然存在.
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