A COMPARISON OF THE STATISTICAL SECULAR VARIATION RECORDED IN SOME LATE QUATERNARY LAVA FLOWS AND SEDIMENTS, AND ITS IMPLICATIONS

Paleomagnetic results from late Quaternary sequences of lava flows, wet sediments, and dry sediments are used to investigate the long-term statistical behavior of the Earth's magnetic-field secular variation. Two statistical parameters, DELTA I anomaly (average site inclination) and virtual-geomagnetic-pole angular dispersion, are estimated from these data sets. Comparison of the late Quaternary statistical results with similar statistical estimates for the last 5 million years, on average, indicates that the late Quaternary global pattern of DELTA I anomaly is unchanged (self-stationary) from its 5-million-year average, but that the late Quaternary global pattern of angular dispersion is significantly different (nonstationary) from its 5-million-year average. Refs.