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

关键词：

D O I：

暂无

中图分类号：

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.

引用

页码：673 / 674

页数：1

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