In GAD we trust

被引：0
|
作者：
Joseph G. Meert
机构：
[1] Gainesville,Joseph G. Meert is at the Department of Geological Sciences at the University of Florida
[2] Florida 32611,undefined
[3] USA. jmeert@ufl.edu,undefined
来源：
Nature Geoscience | 2009年 / 2卷
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D O I：
暂无
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学科分类号：
摘要：
Palaeomagnetists' basic assumption that Earth's magnetic field is a GAD, that is, a geocentric axial dipole, has been challenged by anomalous magnetic data from ancient Canadian basalts. At a closer look, fast continental drift could explain this anomaly.
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页码：673 / 674
页数：1
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