Is 600 Myr long enough for the random palaeogeographic test of the geomagnetic axial dipole assumption?

被引：17

作者：

McFadden, PL ^{[1
]}

机构：

[1] Geosci Austr, Canberra, ACT 2601, Australia

来源：

GEOPHYSICAL JOURNAL INTERNATIONAL | 2004年 / 158卷 / 02期

关键词：

geocentric axial dipole hypothesis; palaeomagnetism;

D O I：

10.1111/j.1365-246X.2004.02321.x

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

A simple analysis suggests that a time interval of more than about 5000 Myr is needed for the random palaeogeographic test to be effective in assessing the geomagnetic axial dipole assumption. This time is so long as to render the test ineffective. Consequently, intervals of 600 Myr should be recognized as providing only a small sample that is likely to be biased towards low-inclination values.

引用

页码：443 / 445

页数：3

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