IS 600 MYR LONG ENOUGH FOR THE RANDOM PALAEOGEOGRAPHIC TEST OF THE GEOMAGNETIC AXIAL DIPOLE ASSUMPTION?

dc.contributor.author	McFadden P.L.
dc.date.accessioned	2022-09-24T04:26:13Z
dc.date.available	2022-09-24T04:26:13Z
dc.date.issued	2004
dc.identifier	https://elibrary.ru/item.asp?id=7563025
dc.identifier.citation	Geophysical Journal International, 2004, 158, 2, 443-445
dc.identifier.issn	0956-540X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38734
dc.description.abstract	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.
dc.subject	GEOCENTRIC AXIAL DIPOLE HYPOTHESIS
dc.subject	PALAEOMAGNETISM
dc.title	IS 600 MYR LONG ENOUGH FOR THE RANDOM PALAEOGEOGRAPHIC TEST OF THE GEOMAGNETIC AXIAL DIPOLE ASSUMPTION?
dc.type	Статья

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