Geomagnetic secular variation and the statistics of palaeomagnetic directions
Publication date
2011
Authors
Deenen, M.H.L.
Langereis, C.G.
Hinsbergen, D.J.J. van
Biggin, A.J.
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Advisors
Supervisors
Document Type
Article
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(c) UU Universiteit Utrecht, 2011
Abstract
In this study, we examine the role of palaeosecular variation (PSV) in the use of statistics for
palaeomagnetic studies, and we provide new reliability criteria for palaeomagnetic poles or
directions.We first conclude that Fisher statistics should not be applied to average palaeomagnetic
directions but to virtual geomagnetic pole (VGP) distributions instead.
Secondly, we strongly advocate that typical properties of geomagnetic field behaviour are
taken into account in the assessment of palaeomagnetic data sets. The latitude-dependent
properties (E, S, k) provide useful guidelines for the reliability of a palaeomagnetic data set. A
reliable assessment of these properties depends on the (sufficient) number of palaeomagnetic
samples being taken. Therefore, as an additional instrument of assessing data sets, we provide
a N-dependent A95 envelope, bounded by an upper limit A95max, and a lower limit A95min
that helps to ascertain whether or not a distribution has sufficiently well-sampled PSV and
therefore geomagnetic field behaviour. Applying these criteria is indispensable for studies
of geomagnetic behaviour, or for studies aiming at using TK03.GAD for inclination error
correction through the elongation/inclination (E/I) method. For palaeomagnetic studies aimed
at geological reconstructions, they form helpful guidelines and increase the confidence in the
rocks having faithfully recorded the field.
An analysis of published Eastern Mediterranean data shows that the vast majority of studies
do not conform to the Van der Voo criteria, in particular with respect to N and A95. We have
provided criteria that are on the one hand more lenient (lower N may still provide relevant
information), and on the other hand more strict (for high N the criterion of A95 < 16° should
be adapted to a requirement of lower A95, e.g. A95 < 5° for N > 80).
Keywords
Palaeomagnetic secular variation, Palaeomagnetism applied to tectonics, Palaeomagnetism applied to geologic processes