CORDIS Project
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This project aims to investigate marine magnetic anomalies to construct plate kinematic models for the Cretaceous normal superchron, enhancing our understanding of tectonic movements and their relationship with mantle convection. The research will utilize marine magnetic records to analyze past plate motions in various…
Marine magnetic anomalies constitute the backbone of plate tectonic studies.
Together with the known time scale of past polarity reversals of the geomagnetic field, these anomalies can be used to date the oceanic crust.
However, periods of several tens of million years (Myr), when the polarity of the geomagnetic field remained stable (i.e., superchrons), lack prominent magnetic anomalies and therefore prohibit the construction of plate kinematic models.
Thus far, internal anomalies formed by pas…
BEN-GURION UNIVERSITY OF THE NEGEV
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