A study of the time-averaged paleomagnetic field for the last 195 million years
During the last decade a great deal of paleomagnetic results have accumulated, and their accuracy and reliability have been increased significantly by improved demagnetisation techniques. In the present thesis all available paleomagnetic data have been analysed for the purposes of providing more understanding of characteristics of the geomagnetic field through geological time. Also, physical implications for geodynamo theory have been sought! As preparatory procedures, data selection,...[Show more]
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