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电动的莫霍 (Moho) 是一个电动的莫霍.

A G Jones1, I J Ferguson

  • 1Geological Survey of Canada, Ottawa, Ontario. ajones@NRCan.gc.ca

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|February 24, 2001
PubMed
概括
此摘要是机器生成的。

地震数据揭示了地-地幔边界,或莫霍罗维奇不连续性 (Moho),但电气研究尚未得出结论. 来自加拿大的新电磁数据.

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科学领域:

  • 地质物理学 地质物理学
  • 地震学 地震学
  • 电磁主义 电磁主义

背景情况:

  • 莫霍罗维奇不连续性 (Moho) 标志着地球地-地幔边界,由地震速度变化确定.
  • 之前的电磁研究没有在Moho检测到相应的导电率变化.
  • 实验室测量表明Moho的导电性对比,这在实地研究中没有观察到.

研究的目的:

  • 为了研究Moho深处的电磁信号.
  • 在地和地幔边界的地震和电磁观测之间的差异调和.
  • 为了探索一个异常的石坑下方最上层地幔的电特性.

主要方法:

  • 来自加拿大北部的Slave石坑的电磁数据分析.
  • 观察到的导电率与地幔岩石上的实验室测量结果的比较.
  • 利用奴隶的异常低地电导率进行高分辨率的Moho成像.

主要成果:

  • 在莫霍深处检测到电导率的明显阶段变化.
  • "奴隶"石坑表现出极低的地总导电率 (<1西门子).
  • 莫霍河下方的上层地幔导电性比奥利文研究预测的高出两倍.

结论:

  • 电磁方法可以解决Moho的导电率变化.
  • 最上层地幔的高导电性表明一个连接的导电相.
  • 这一发现挑战了现有的地地幔边界组成和特性模型.