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f Potential Field Grids in a Plate Tectonic Context - Animation and Re-Evaluation of Continental Margin Evolution
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, 57th EAGE Conference and Exhibition, May 1995, cp-90-00117
- ISBN: 978-90-73781-06-1
Abstract
Gravity and magnetic data have played an important part in de fining plate tectonic models over the years. Magnetic anomalies in the oceans are important age markers and define how lithospheric plates have to be reconstructed with time; marine gravity data on the other hand (along with bathymetric information) show the fracture zones along which platen have moved relative to each other through time.