Russian Journal of Earth Sciences
Vol 1, No. 2, December 1998
Translated February 1999

Neogaean paleomagnetism constraints on the processes at the core and surface of the Earth

D. M. Pechersky

United Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia

Introduction
Part 1. Geomagnetic Field in the Neogaea

Geological Time Scale
Geomagnetic Polarity Behavior
Fractal Analysis of the Reversal Scale
Wavelet Analysis
Summary Amplitude of Paleovariations in the Geomagnetic Field Direction.
Variation in the Paleointensity (Modulus of the Field Intensity)
Main Features of the Geomagnetic Field Behavior in the Neogaea

Part 2. Comparison of Processes at the Core and Earth's Surface

Changes in the Organic World and Geomagnetic Reversal Frequency
Horizontal Velocities of Continental Plates
Comparison Between Continental Plate Velocities and Geomagnetic Reversal Frequency in the Neogaea
Generalization of results

Conclusion
Acknowledgment
References

Load files for print and local use.

This document was generated by TeXWeb (Win32, v.1.0) on April 7, 1999.

Neogaean paleomagnetism constraints on the processes at the core and surface of the Earth

Contents