Major peculiarities of the bottom topography and anomalous magnetic field near the Bouvet Triple Junction were established. The three-dimensional modeling of the parameters of the inverse magnetoactive layer allows one to reconstruct a comprehensive geochronology of the bottom and to show the unstable character of the junction area of the American, African, and Antarctic plates during the past one million years.
Comprehensive geomagnetic research on the Triple Junction near Bouvet Island
Zitellini;Ligi;Ma;
1997
Abstract
Major peculiarities of the bottom topography and anomalous magnetic field near the Bouvet Triple Junction were established. The three-dimensional modeling of the parameters of the inverse magnetoactive layer allows one to reconstruct a comprehensive geochronology of the bottom and to show the unstable character of the junction area of the American, African, and Antarctic plates during the past one million years.File in questo prodotto:
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